FIELD PROCEDURES (See “Data Sheets” section for sample data sheets.) KNOW BEFORE YOU GO SAFETY ..........................................................................................................................1 TEAM RHYTHM AND STREAM ETIQUETTE ........................................................................7 ANTI-CONTAMINATION PROTOCOL .................................................................................9 QUALITY ASSURANCE… ................................................................................................ 11 COMPASS USE .............................................................................................................. 13 STREAMKEEPERS BASIC QUARTERLY MONITORING WATER CHEMISTRY—GENERAL GUIDELINES ................................................................. 15 AIR TEMPERATURE ....................................................................................................... 17 TURBIDIMETER: HF-DRT 15CE ...................................................................................... 19 TURBIDIMETER: HACH 2100P ...................................................................................... 23 pH: YSI 60 ................................................................................................................... 27 MULTIMETER: YSI-85 ................................................................................................... 33 MULTIMETER: HYDROLAB QUANTA .............................................................................. 38 FLOW ........................................................................................................................... 47 PHOTOS ....................................................................................................................... 57 CAMERA USE ................................................................................................................ 61 FISH AND WILDLIFE SIGNS ........................................................................................... 65 NOXIOUS WEEDS ......................................................................................................... 69 BIOLOGICAL MONITORING (OTHER THAN FISH, WILDLIFE & WEEDS) BENTHIC MACROINVERTEBRATE SAMPLING .................................................................. 71 GRAB SAMPLING FOR LAB ANALYSIS (BACTERIA, NITRATES, ETC.) ................................ 77 PHYSICAL HABITAT MONITORING NOTE: All physical habitat parameters other than Bank Stability and Gradient were mothballed in 2005; see “Physical habitat sampling” at http://www.clallam.net/streamkeepers/html/program_planning.htm BANK STABILITY ASSESSMENT...................................................................................... 81 GRADIENT .................................................................................................................... 83 ESTABLISHING CROSS SECTION MONUMENTS............................................................... 85 BANKFULL: WHAT IT IS AND HOW TO LOCATE IT ......................................................... 89 CROSS SECTION SURVEY .............................................................................................. 91 LARGE WOODY DEBRIS ................................................................................................ 95 EROSION/REVETMENT SURVEY ..................................................................................... 97 POOLS SURVEY............................................................................................................. 99 PEBBLE COUNT........................................................................................................... 101 CANOPY CLOSURE (SINGLE POINT) ............................................................................. 103 CANOPY TYPE PERCENTAGES (REACH-WIDE) .............................................................. 105 CONIFER STEM COUNT ............................................................................................... 107 NEW PROJECTS, TEAMS & SITES SAMPLING PLAN DESIGN ............................................................................................ 109 NEW SITE/REACH ESTABLISHMENT ............................................................................. 111 SAMPLING SITE SKETCH MAP...................................................................................... 113 REACH MAP ................................................................................................................ 115 Field Procedures 15th Edition, 2013 This page is intentionally blank for printing. SAFETY This is Chapter 1 because it’s Job 1. Keep the following points in mind: • • • • • • • • • • • • • Safety is a group effort: We recommend that you don’t go out alone (depending on circumstances) and make sure somebody knows where you’re going and when you expect to be back. Emphasize safety with your entire group, and watch out for each other. Precautionary principle: If you are in doubt as to your ability to safely collect a sample, don’t do it! Be aware of your physical limitations and those of the rest of your team, and the difficulty of collecting samples at certain locations under certain conditions. County Incident Reports (attached): Turn one in anytime there’s an accident or near-miss. Cell phones: We can provide you with an emergency 911-cell phone on request, but they are not always reliable out in the woods. • If you have a cell phone, give your number to SK staff. • Before each outing, make sure your cell phone is fully charged and that you’ve updated your roaming capability (see your manual). • Exchange cell phone numbers with your fellow team members and re-confirm them each time you go out. Keep your cell phone on during the entire outing. • Upon reaching the site, determine the nearest location cell phone service can be accessed before beginning work. (If not at the site itself, try the top of the bank or ridge, a nearby clearing, or the place where you parked.) Record this information for the SK staff, who will enter it into the site-description information. Check this each time you go out. • Team leaders should predetermine emergency services cell phone GPS capability for the site where the team will be located; site descriptions in your forms folders will include latitude, longitude, and horizontal datum—the essentials required by emergency services. • Walkie Talkies are also available for cases where volunteers separate from one another. Orientation: If you don’t know the area, take a good map with you. Traffic: Be careful when pulling off the road and leaving your car. If you are working near a road, wear orange vests (which we can supply) or other bright clothing. Medical conditions: Let your staff and team know if you have any special medical conditions, such as heart problems, diabetes, asthma, or extreme allergies. If your emergency contact number is other than your home phone, let your teammates know. BRING ANY NEEDED MEDICATIONS WITH YOU INTO THE FIELD, AND LET THE REST OF YOUR TEAM KNOW WHERE YOU KEEP THEM. Warm-up: Stretch before stream walking, especially quadriceps, calves and hamstrings. If you’re limber, you’ll find it easier to move when faced with sudden loss of footing. Awareness: Keep your eyes moving, scanning the stream in front of you when walking and looking around you when monitoring. (Note that jacket hoods block peripheral vision and ballcap bills block hazards overhead.) Be conscious of your body placement as you rest or write— you want to be able to see around. Make a habit of looking for tracks. Walking: Boots with felt bottoms or corkers are the safest. Many boots do not offer much support, so if you have weak ankles, wrap them for stability. Walking sticks have numerous uses: third leg, water depth/substrate tester, brush whacker, balancing aid, and weapon. Polarized glasses will help you see the creek bottom. Carrying equipment: The equipment bags are bulky and heavy; if your access trail is long or arduous, you may want to repack stuff into frame backpacks (available at the office). Fatigue: Note your energy level and those of your teammates. Know when to quit. High flows: In higher flow situations plan your stream crossings at an angle, allowing the water to “carry” you to your destination. But don’t go in at all if the water’s too high and/or Field Procedures 1 15th Edition, 2013 SAFETY • • • • • • • • • deep: The “rule of 10” states that you shouldn’t go into water where velocity (ft/sec) X depth (ft) ≥10. If you can’t wade across, you can do many of the field procedures from the bank. Log Jams: All log jams, no matter how small, have the potential to cause injury—avoid them if possible. If you have to walk on them, choose the most stable and safe parts. Beware of bare logs or alders, which are slippery and may be rotten. Make sure your footing is on a stable log before resting all your weight on it. Attempt to have an escape plan if a particular log shifts. Avoid pulling yourself up via attached branches. Bad water: Our creeks are not all pristine, and even those that seem so might surprise you! Avoid hand-mouth contact; use gloves and hand-sanitizer provided in your kit. Hazardous materials: The most dangerous materials we use are alcohol and glass cleaner (which you should have heard about during volunteer orientation), but you may find other hazardous materials at your sites—broken glass, needles, human/animal wastes, etc. Brush: Some parts of the stream may be very brushy or worse. Help each other to avoid getting tangled or prickled, and work around what you have to. Also beware of some of the more dangerous plants, such as poison hemlock and giant hogweed—you’ll learn about these during Noxious Weed training. Protective gear: Be prepared for rain, wind, and cold. For cold, bring a thermos or a St. Bernard, plus extra layers of clothing, rain gear, and a warm hat. For heat, bring a hat, sunblock, and plenty to drink. For brush and biting insects, long pants/sleeves and rubber garden gloves are good. We stock garden gloves in the field kits, but bring your own if you don’t wear shared apparel. Rain: If it begins to rain heavily, thunder, lightning, or hail, get out of the stream and into your car. If it seems to be a passing storm, try waiting it out and then returning to the stream. Note on your field form the time you left and returned, and about how much rain fell. Keep an eye on water levels if it has been raining anywhere in the watershed. Dogs: Use your best judgment if a menacing dog comes your way. Running is not the best reaction. Talk to the dog calmly and call for the owner. Bees: Bees may nest along stream banks, in the ground, and in hives in the trees. Watch for nests or “sentinel” bees. If you see bees, avoid them and notify your teammates. Our First Aid kits include “sting-ease” sticks which alleviate both stings and nettles. You might also wish to carry the antihistamine diphenhydramine (Benadryl) in liquid form, to help alleviate a severe allergic reaction, and consider asking your physician for a prescription for Epi-pens that you can bring into the backcountry with you, to treat yourself or anyone else who might have an anaphylactic reaction to a bee-sting. Though rare, this is a potentially fatal event. Mushrooms: Yes, mushrooms—stay away from these! Some of them can even poison a person through the skin! First Aid/CPR: There is a First Aid kit in each field kit with a variety of supplies and a First Aid booklet; see the list at the end of this chapter. We urge you to get trained in First Aid/CPR. Streamkeepers periodically offers a free First Aid/CPR training which is somewhat adapted to our special conditions, but other organizations, such as Red Cross, also offer these courses on a regular basis. We stock a CPR mask in our first aid kits, but it’s not a top-quality one such as a Laerdal; you may want to purchase one of these. (Note that as of November 2005, the American Heart Association advises that if you don’t feel comfortable doing CPR with rescue breaths, chest compressions alone can be effective.) Wilderness First Aid books may be borrowed from the office. Field Procedures 2 15th Edition, 2013 SAFETY Seasonal Safety Issues Monitoring in Wet & Cold Weather Conditions 1. FREEZING TEMPERATURES AND YOU: Cold, wet conditions call for extra precaution against hypothermia; keep an eye on your teammates, particularly if it's wet. (And even if it's not raining, the vegetation will probably be wet enough to merit chest waders if you have them.) If you see someone with purple lips slurring their words, warm them up or send them home. Don't hesitate to use the space blanket in the first aid kit. 2. FREEZING TEMPERATURES AND EQUIPMENT: Don't leave the "clean bag" in your car or garage overnight if it looks like it will freeze. The turbidity standards can be ruined if they freeze, so if it's really cold, you might have to carry them in your pocket on monitoring day. The YSI meters will not function properly below 23°F (-5°C), and your teammates probably won’t either, so if it’s that cold, postpone till a warmer day. 3. WAYS TO MAKE MONITORING EASIER: a. GLOVES: The big orange gloves (in the plastic tub) are the best way to keep your hands warm if you have to hold an electronic probe underwater for a while. Short of those, the other gloves in the kit will also help somewhat. b. DRY WORK AREA: We have big beach umbrellas available, along with rebar anchors, if you want a dry space for people and/or equipment. And we have an extra tarp we can loan out. c. WATER CHEMISTRY IN THE CAR: The next-to-last page of the Water Chemistry protocol has a box entitled “Alternative Water-Chemistry Procedures for Poor Conditions”. Check it out! 4. FLOOD CHANGES: Due to flooding, many of your sites might have changed quite a bit or become hard to access. It would be a good idea to scout your sites beforehand, to make sure there aren't "issues" to be resolved. You might want to bring a hand saw, axe, etc. If the site has changed drastically and you have a detailed reach map of it, you might want to draw a new one. See the “Site Sketch Map” or “Reach Map” chapters for details. Summer Safety Remember the hazards of summer: heat stress, dehydration, sunburn, and biting insects. Yellow Jackets: • Reactions to a sting can be immediate or delayed, toxic and/or allergic, including deadly anaphylactic shock. Streamkeepers cannot supply any medications in our first aid kits, but we encourage individuals to do so, particularly for anaphylaxis; see “Items Recommended to Bring Yourself” below. • Yellow jackets do not leave their stinger. They can sting multiple times. If you are stung and a stinger remains, chances are that you were not stung by a yellow jacket. • When they sting, they release a pheromone that alerts others in the nest to come and help defend the nest - hence the sudden appearance of many angry insects when a moment ago there were none. • When you run afoul of a yellow jacket, cover your face with your hands and move swiftly away. No running and no flailing - although an instinctive response, these actions aggravate them. • Bright colors and floral patterns indicate to them that you may be food. So do fragrances. Field Procedures 3 15th Edition, 2013 SAFETY Spiders and Ticks and Mosquitoes: You may not feel the sting or bite when it happens, but you’ll probably soon notice swelling, redness, itching, or even pain. Some people have to worry about much more than that, though. If you’re allergic to bites or stings, they could cause hives, dizziness, stomach cramps, or nausea. In rare cases, people feel weak or have trouble breathing or swallowing. In the worst instances, that can lead to unconsciousness, and even shock or death. There are insects like black flies and tiny red chiggers whose bites cause serious itching. They rarely lead to worse problems, however. Spider bites are generally harmless, with a few exceptions, such as the bite of the black widow spider. This poisonous spider is glossy black with a red hourglass mark on the stomach. It measures just one-half inch in diameter, and lives in woodpiles, sheds, and basements. The bite itself may not hurt, but it could cause bad stomach pain and cramps, breathing difficulty, and possibly nausea, sweating, twitching, shaking, and tingling in the hand. See a doctor immediately for black widow spider bites. Also be alert for brown recluse spiders. They’re smaller than black widows and have a white pattern that looks like a violin on their backs. Their bites can be painful and cause some of the same reactions as black widows, but they’re not as dangerous. Tick bites are a particular concern. Ticks are tiny bugs that live in tall grass or shrubs and often ride on deer, dogs, mice, or people. Some ticks carry serious illnesses such as Rocky Mountain spotted fever and Lyme disease. You need to identify and treat these illnesses early. • Check yourself and your clothing for ticks when you finish an outdoor job. If one of these tiny insects is on your skin, remove it quickly. Grab the tick with fine-tipped tweezers, getting as close to the skin as possible. Then pull it straight up with steady even pressure so you get all its body parts. If you can’t remove the tick yourself, get medical help to do so. Once it is out, wash the area gently with water and apply rubbing alcohol. • See a doctor immediately if you develop a large red spot from the bite or if you develop swelling, fever, joint pain, or flu-like symptoms within a few weeks. Physicians can treat tickborne diseases with antibiotics. However, fast treatment is essential for maximum effectiveness. Mosquitoes can carry a number of dangerous and deadly diseases, including malaria, dengue and yellow fevers, several variations of encephalitis, and West Nile virus. Protect yourself from insect-borne diseases by following these tips: • Wear light-colored snug clothes. Don’t use perfumes or colognes. • Use insect repellent on skin and clothes. Follow label warnings. • Get immediate medical attention for a black widow spider bite and difficulty breathing or swallowing. • Check for tiny ticks after all outdoor work. • Remove ticks immediately with fine-tipped tweezers. Grab close to skin, pull entire body straight up. Get medical help if you can’t remove it. Then wash with water and cleanse with rubbing alcohol. • Get prompt medical attention if a tick bite causes a red spot or if swelling, fever, joint pain, or flu-like symptoms develop. Field Procedures 4 15th Edition, 2013 SAFETY Field Procedures 5 15th Edition, 2013 SAFETY Streamkeepers First Aid Items Note: always ask for permission to treat first. If patient is not responsive, consent is implied if you are acting with good intentions and within your level of training, particularly if you are acting to prevent the patient’s death before medical help arrives. Items in Streamkeepers First Aid Kits Item CPR Microshield Emergency blanket Quantity 1 1 LED Light (reg. kits) Sting relief tube (reg. kits) 1 1 Cake icing tube w/instructions 1-4.25 oz Cold Pack Gloves – large Gloves – medium Triangular Bandage Adhesive Tape Stretch Bandage Ace Bandage Moleskin/Molefoam Abdominal Pad (5in x 9in) 1 At least 2 pair At least 2 pair 1 1 roll 1 roll 1 1 pad 1 Gauze Sponges (4in x 4in) Non-Adherent Sterile Pad Antiseptic Wipes Misc. Band-Aids Compound Benzoin Tincture Swab Safety Pins Tweezers Chrome Snippers Biohazard Bags First Aid Report Form 1 pkg 2 5+ Many 1 Pencil Emergency First Aid Booklet 1 1 3 1 1 Pair 2 2 Forms Comments Offers protection when giving rescue breaths For hypothermia, but can also be used as a tarp or to scare away animals May give some relief from stinging nettles as well as insect bites For hypoglycemic (low blood sugar) episodes; take 1 Tbsp., wait 15 min., repeat as often as needed To maintain a barrier vs. blood-borne pathogens For making slings or other wraps For direct application to profusely bleeding wounds; place additional pads on top of one another as needed To clean wounds once bleeding has stopped Use on skin surrounding wound if wet conditions make bandages hard to stick To cut away clothing to perform first aid For materials contaminated with bodily fluids These can guide you to things to look for while waiting for emergency assistance Items Recommended to Bring Yourself 1. High-quality CPR mask with a good seal and breathing tube, such as Laerdal Pocket Mask (if you’re prepared to perform rescue breathing). 2. Ibuprofen (to relieve pain, inflammation, headache): take up to 4 x 200 mg. 3. Chewable aspirin for angina (heart stress): up to 648 mg, chew or crush & place under tongue; do not use if internal bleeding is suspected 4. Antihistamine, e.g., diphenhydramine (Benadryl), preferably in dissolving strip form; for allergic reactions including anaphylaxis (see below). 5. Epi-Kit (bee-sting kit) with injectable epinephrine: for anaphylaxis; requires a prescription—your doctor will ask you to prove that you know when and how to use; expensive; must be accompanied by anithistamine (see above) or the patient will probably “rebound” after a few minutes when epinephrine wears off; they may “rebound” anyway, so be prepared to adminster a second injection; Patient must be transported to nearest emergency room for further treatment. Field Procedures 6 15th Edition, 2013 TEAM RHYTHM AND STREAM ETIQUETTE QUARTERLY MONITORING SEQUENCE This is roughly the way things work each quarter to get a team’s monitoring done. Different people on the team might take on different tasks. • Decide on monitoring dates with your team and reserve a field kit— earlier is better! • Inventory field kits for completeness before taking them out. (Generally, our office • Store your kit safely when not in use, and do not leave the “clean bag” in your car or garage volunteers will have done the inventory for you—check this on the inventory sheet.) • • • • • • • • during extreme hot or cold temperatures, or the equipment or chemicals might fail to function properly and possibly require costly replacement. Visit all sites (from highest to lowest) on a given stream on the same day. This is important for certain types of upstream/downstream comparisons. If you have to spread out the visits over more than one day, please note on your data sheets whether there was a precipitation event (and how many inches) in between. If a site has no flow, you should still fill out a data sheet; zero flow is important information. You can still look for wildlife, weeds and take photos. At a given reach, begin with fish and wildlife observations—you’re most likely to see things before you’ve mucked around very much. Be sure to take all chemical tests and macroinvertebrate samples upstream of any places where you have walked in the creek. Update your reach map or sketch map as needed, preferably with a pencil; initial and date any changes you make; and describe these changes on your field data sheet, along with a note for staff to recopy the updated reach map for the office file. If the changes in the reach are substantial, plan a day with your team to redraw the map. Before leaving your site, check to see that you’ve packed all the equipment. (Did you get the thermometer that you hung up in that tree?) Turn in your equipment on time. Remember to: • Leave notes for staff if equipment needs maintenance, replacement, or calibration. • Turn in your volunteer hours sheet, completely filled out for each volunteer. • Check over all field sheets for completeness and clarity before turning them in. • If possible, leave anything wet out to dry. • If you have time, please check in your field kits using the inventory sheets on the clipboards. (Otherwise, our office volunteers can often perform this task.) Office Etiquette: Please don't come inside the Courthouse wearing muddy boots. If it’s inconvenient to change, you can just take your boots off and leave them outside the entrance, then come inside in your stocking feet. Also please don’t prop open the back door; when you get alcohol, borrow a passkey from a staff person so you can return to the building. LEGAL AND COURTESY ISSUES • • Trespassing: Be careful not to trespass. We have permission to monitor at all of our regular monitoring reaches, but that does not give you the right to walk all up and down the stream. In Clallam County, even some parts of some stream bottoms are privately owned. Neighborliness: Where we do have permission to access private property, remember that we are guests and ambassadors for the Streamkeepers program. When you see people out in the field, wave and say hello. Let them know about the important work you’re doing. Business cards are in the field kit, and your Volunteer Handbook serves as a rather substantial “greeting card.” If a property owner asks you to do something or not do something when on their Field Procedures 7 Revised 1/15/2014 TEAM RHYTHM AND STREAM ETIQUETTE • property, please let staff know so we can enter that information into the database and print it out for future samplers. Illicit Discharges: If you see (or smell) anything other than rainwater entering any creek, ditch or storm water conveyance, report it to Streamkeepers. CARING FOR THE CRITTERS All streams support a large array of interconnected communities—from fish to invertebrates to lower organisms such as algae. Walking in a stream will cause some disruption to these links. The key is to be aware and minimize any damage. If possible, walk along the banks (this includes exuberant canine companions!). When you have to walk in the stream channel, be aware of your travel path. Virtually any time of year, some type of salmonid spawning activity could be taking place in a stream. In general, the North Olympic Peninsula spawning seasons are as follows: August September October November December January February March pinks cutthroat chinook, chum steelhead April May June coho After spawning, eggs will develop at different rates depending on water temperature. Ninety-five days is the average from egg fertilization to first feeding of fry. Detection of developing eggs under a blanket of gravel can be a challenge. Chinook and coho build classic redds that look like pockets (pits) in the gravel with mounds (tailouts) of clean gravel behind them. The eggs are in the tailouts, which can extend 1 - 2.5 meters downstream. Salmon that spawn en masse, such as pinks and chums, tend not to build redds that are distinctive other than cleaned gravel. Also, high flows can smooth out the contours on these sites. Knowledge of substrate size, spawning location, and spawning characteristics of salmonid species may help minimize potential damage. Below is a generalized chart describing salmonid redds: SPECIES Chum Pink Sockeye SPAWNING GRAVEL SIZE Small Small-Mid Small REDD LOCATION Coho Cobble (tennis to basketball size) Small-Mid Steelhead Small-Mid Typically low in river systems Typically low in river systems Along lake shores or adjacent streams Mainstem rivers and lower tributaries Side channels, tribs, margins of rivers Mainstem and tribs Cutthroat Small Tribs and small streams Chinook SPAWNING CHARACTERISTICS Mass spawning is typical Mass spawning is common Mass spawning Distinct redds Distinct redds Distinct redds or nests (small redds) Mini redds Special thanks to Theresa Powell & Camille Speck, biologists with the Washington State Department of Fish & Wildlife, for their valuable input on this chapter. Field Procedures 8 15th Edition, 2013 ANTI-CONTAMINATION PROTOCOL The State is concerned about the spread of exotic invasive plants and animals into our streams due to people like us mucking around at one site and then visiting another. For that reason, they’re asking us to take measures to prevent cross-contamination. Until we work out a more detailed set of instructions for Streamkeepers, here are some general rules to follow (Parsons 2013): 1. Instead of doing multiple sites on a stream from downstream to upstream (our former procedure), please go from upstream to downstream. However, in some cases it’s OK to go from downstream to upstream to avoid contaminating samples with your own upstream movement in the stream: A. Where sites are very close together (as sometimes is the case for grab sampling). B. Where the disturbance-level of the stream is clearly uniform (as in a highly-impacted urban area). C. If it’s critically important that you not disturb the stream upstream of where you’re sampling, follow the decontamination protocol closely with your boots and other things that enter the stream, and you should be safe to go from downstream to upstream. 2. Anything that enters the water at a site (boots, flow meter wands, Surber samplers, etc.) needs to be treated as follows when leaving the site: A. Thoroughly inspect whatever has contacted the water and use a brush to remove all dirt, debris, and organisms. B. If you’re not sure you’ve removed everything or have felt boot bottoms, spray thoroughly with hydrogen peroxide, or a cleaning agent with quaternary ammonia compounds (such as Formula 409 regular or Simple Green Pro 3) and enclose in a plastic bag for at least 15 minutes (10 minutes for quaternary ammonia products), while traveling to your next site. C. If you’ve used a quaternary cleaning agent, you’ll have to rinse those items away from the stream before sampling at the next site. You can use the tub in the field kit to carry water from the stream. D. A decontamination kit consisting of a brush, disinfectant, big plastic bags and ties is in the Streamkeeper field kit’s “dirty bag”. 3. If you can avoid going into the water, please do (for example, when doing grab sampling). But check all equipment that entered the water. 4. If possible, take multiple pairs of boots to make the decontamination process go more smoothly. For more information, see this web page from the Washington Dept. of Ecology: http://www.ecy.wa.gov/programs/eap/InvasiveSpecies/AIS-PublicVersion.html Field Procedures 9 Revised 1/15/2014 (This page is intentionally blank for printing.) Field Procedures 10 15th Edition, 2013 QUALITY ASSURANCE… …or, How to Get Your Data into the Database & Not the Dustbin! In order to gather data that others will trust and use, Streamkeepers performs its quarterly monitoring procedures under a Quality Assurance Project Plan that has been approved by the Washington State Department of Ecology. In order to get approval on this plan and its implementation, we need to follow certain procedures to maintain a consistent quality of data. This chapter outlines some of those procedures. GROUND RULES FOR MONITORING • • • • Rule #1: Follow the written protocols. They are the key to data credibility. If you have questions about the correct procedure or interpretation, ask your team leader or note your questions on the data sheet or in a separate note to program managers. Take field notes. Include weather observations, appearance of the reach or water, equipment problems or substitutions, and any modifications to the written protocols. Think about your data and whether it seems reasonable. Compare it to your common sense, past data at that site, data from similar sites, or the typical data ranges given to you on your data sheet. If you are at all uncertain about the data you’ve taken, try taking the data again. Note what you did, and your results, on your data sheet. If you’re getting tired and sloppy, go home—no data is far better than junk data. HANDLING THE ELECTRONIC EQUIPMENT Our field kit’s electronic meters require special care to work properly and last a long time: • Don’t drop them or the bag they’re carried in. Remember to turn them off when you’re finished, and set them in the bag in such a way that they won’t turn on accidentally. • Cables are most vulnerable near their junctions. Avoid putting too much stress on them at these points—for instance, by kinking, pinching, or yanking on them where they meet the probe or meter, or by storing them in such a way that they are kinked. • When the temperature is below freezing, you must take extra precautions about storage and use: • The YSI meters should not be stored or used in temperatures<23°F (-5°C). • Don’t let your purified water freeze! • The turbidity reference vials go bad and have to be replaced if they freeze. If you're out in the field on a below-freezing day, keep all 3 turbidity vials in your pocket to keep them warm--and remove anything from your pocket that might scratch them. RECORDING DATA • • • • • • When signing in on the top page of a data-sheet packet, all samplers should include their full initials plus full last names. For each parameter, one sampler will initial, indicating responsibility for the data. This should be a person who has been trained by a staff person or attended a training session on that parameter. If none of the samplers have been trained, note that on the data sheet. Fill in all blanks on the data sheets. Remember especially the lines at the top of each page where you enter the name of the site and the date; otherwise, your data could get lost! If you forget your site name (usually, stream name + stream miles), there should be a list on your field forms folder. Or write the stream name plus a description of the site location. Write legibly. Your fellow volunteers have to enter your data into the database! For any procedure, if you looked for whatever the data sheet asks for (fish, wildlife, weeds, flow, etc.) and found none, write “NONE” and your initials on the data sheet. Field Procedures 11 Revised 1/15/2014 QUALITY ASSURANCE • Record all times using 24-hour (military) notation, whereby: • 8:00 a.m. = 0800 • Noon = 1200 • 12:30 p.m. = 1230 • 1:00 p.m. = 1300 • 8:00 p.m. = 2000 • Midnight = 0000 STREAMKEEPERS’ NUMBER-ROUNDING CONVENTION Your protocols and field sheets will tell you how many decimal places to include when you record numbers. Sometimes, our electronic meters will give you more decimal places than you are supposed to record. Please record only the number of decimal places asked for in the protocol—if you record more decimal places, you’ll cause problems for the volunteers who do data-entry. When rounding a decimal that’s halfway between, we do NOT simply “round up,” because that would bias the data. Instead, Streamkeepers’ rounding convention is summed up by the phrase, “If halfway, round to the nearest even.” Details are below; pay close attention to the “tricky part,” that is #3 & 4: 1. If the figure beyond the last figure to be retained is less than 5, do not change the last figure to be retained. Example: rounding 34.44 to the nearest tenth gives 34.4. 2. If the figure beyond the last figure to be retained is greater than 5, then increase the last figure to be retained by 1. Example: rounding 34.46 to the nearest tenth gives 34.5. 3. If the figure beyond the last figure to be retained is 5 (followed by zeroes or with no following figures)… a) keep the last figure to be retained if it is even, or b) increase the last figure to be retained if it is odd. c) Example: rounding 34.45 to the nearest tenth gives 34.4. Rounding 34.55 to the nearest tenth gives 34.6. 4. If the figure beyond the last figure to be retained is 5, followed by figures other than zeroes, regard the “5” as really greater than 5 and use Rule 2 above. Example: rounding 34.451 to the nearest tenth gives 34.5. This number… 43.64 43.66 43.65 43.75 43.85 43.851 43.855 43.855 43.995 Field Procedures SAMPLES OF STREAMKEEPERS’ ROUNDING CONVENTION: …when rounded to this many decimal …rounds to this places… number: .1 (nearest tenth) 43.6 .1 (nearest tenth) 43.7 .1 (nearest tenth) 43.6 .1 (nearest tenth) 43.8 .1 (nearest tenth) 43.8 .1 (nearest tenth) 43.9 .1 (nearest tenth) 43.9 .01 (nearest one-hundredth) 43.86 .01 (nearest one-hundredth) 44.00 12 15th Edition, 2013 COMPASS USE a bearing. The compass can be used in a number of different ways, as explained below. Streamkeeper volunteers use the compass for two separate operations: either working “from terrain to map” (taking a compass bearing from a given line in the field) or working “from map to terrain” (following a bearing given on a stream reach map). The first operation is used when surveying the stream reach map, and the latter would be used to reestablish your reach lines during future monitoring visits, or to find stream reach monuments after a reach has been established if thick growth or flooding alters the terrain. DEFINITIONS A few definitions are useful for an understanding of compass use: Bearing: The direction from one place to another, measured in degrees of angle with respect to an accepted reference line. This reference is the line to true north. Taking a bearing: To measure the direction from one point to another, either on a map or in the field. THE COMPASS Following a bearing: To set a certain bearing on the compass and then to follow The compass supplied with the field kits has been set to account for the 20-degree east declination for the Peninsula, the difference between the magnetic pole and true north, so all of our readings will reference to true north. Remember to keep the compass level and away from iron and steel objects like belt buckles, rings, rebar, or clipboards when taking that bearing along a line in the field. Boxing the needle: To align the red end of the magnetic compass needle inside the orienting arrow of the compass housing. Triangulation: Taking a bearing to a monument from two different locations. Orienting arrow with red north end Field Procedures 13 Revised 1/15/2014 COMPASS USE USING THE COMPASS FROM MAP TO TERRAIN—To follow a bearing written on your stream reach map to establish a point or line in the field, by setting the bearing on your compass: This method is used to reestablish the baseline or transects in the field, or to find the “zero point” or other landmark based on triangulation from other points. You’ll use the reverse of the procedures described in “From Terrain to Map.” FROM TERRAIN TO MAP—To take a compass bearing from the terrain for your stream map by measuring the direction from one point to another on the terrain: Let’s say you need to determine the compass bearing of your baseline (see Reach Map protocol). 1. Stand at your “zero point” with your tape stretched along your baseline, and orient the body of your compass in exactly the same direction. There are several ways to do this: a) “Lay-along” method (preferred): If you have a tape or string lined up exactly along the line you want to measure, you can lay the compass directly on top of it or next to it, thus assuring that it is pointing in the same direction. b) “Sight-through” method (slow, accurate): open the compass cover to about a 50-degree angle so that you can see the compass dial in the mirror when held to the eye, as well as the tape measure through the slit. c) “Sight-down” method (quick, not accurate): Hold the compass about waist level with the lid away from you. Aim the sighting slit/sighting line on the compass cover down the baseline. 2. To read the compass, “box the needle” by rotating the compass housing so the orienting arrow aligns with the red magnetic needle (see diagram). Read and record the bearing at the index line. Quick Accuracy Reading: Suppose, for example, that you can’t find a rebar monument you put in the year before. Your map notes that the monument is “20 feet at 270 degrees from the corner fence post.” Simply stand at the fence post and turn the compass dial to set 270 degrees at the index pointer. Holding the compass flat open at waist level, box the needle by ROTATING YOUR ENTIRE BODY until the red needle aligns with the orienting arrow. The sighting line will be pointing toward the monument, and you should be able to zero in on it now in the brush. Extreme accuracy reading: Let’s suppose you still can’t find your monument and will have to install a new one. You’ll need to be very accurate in order to get the monument in the same exact place. To do this: • Use the “sight-through” method to find your bearings (see previous section). • Use triangulation to get as accurate a location as you possibly can. This involves locating your spot from two different reference points. Your reach map should have two different reference points for each important monument (see Reach Map protocol), and if you mark the spots indicated by both of these reference points, they should agree with each other. If they don’t, you’ll have to use your best judgment as to where to locate the replacement monument. IF YOU HAVE TO RE-INSTALL A MONUMENT, BE SURE TO NOTE WHICH MONUMENT AND EXACTLY HOW YOU DECIDED WHERE TO PLACE IT. Index line “Boxing the needle” to take a bearing from a line Field Procedures 14 15th Edition, 2013 WATER CHEMISTRY—GENERAL GUIDELINES 3. At that reach, perform each test a second time, as soon as possible after the first, redipping the sample bottle for the turbidity test. You do NOT need to recalibrate between tests. 4. Record and initial results on the replicate section of the data sheet. Overview Our water chemistry data are submitted to the State under the federal Clean Water Act, so our procedures evolve in line with the State’s updated quality-assurance (QA) standards. For a general discussion of the role of data in implementing water cleanup, see www.ecy.wa.gov/programs/wq/303d/index.html Replicate deviation & QA: Our QA plan requires us to take replicates in order to check the precision (consistency) of our data. If your replicate for a given parameter differs widely enough from the original sample, we have to flag ALL the data for that parameter for your team for that season as “Estimated” or “Rejected”. Here are the allowable differences between sample and replicate: Where to Sample When first arriving at a site, you need to think carefully about where and when to perform each monitoring procedure. For water chemistry measurements, you must sample an area upstream of any disturbance by your team. Pick an area where the stream is flowing and appears to be well mixed. Parameter Sampler’s Initials Turbidity (compare ±1 NTU, or the averages) Sum ≥ Difference x 30 Water temperature ± 0.2°C DO concentration ± 0.3 mg/L Conductivity Sum ≥ Difference x 30 pH ± 0.2 pH units If any of your sample/rep differences are beyond the acceptable limits, take further replicates until you have a pair of readings within the limits. Then label the first of the pair your “sample” and the second your “replicate.” On your data sheet, note these extended replicates, as well as any explanations you may have as to why multiple replicates were needed. Depending on the circumstances, we might still have to flag the data. For each test that you perform in this protocol, there is a “Sampler’s Initials” box to the right of the data boxes. Be sure to put all the initials of one sampler taking responsibility for the data; this should be someone who has been properly trained (see “Quality Assurance” protocol). Common Sense and Expected Ranges Please compare your readings with the expected ranges on the datasheet. If you’re outside the expected range, consider resampling or troubleshooting with your fellow samplers. Field Replicates Our quality control plan requires that at one of your team’s sites (or ≥ 10% of your sites if you have >10 sites), you take a second set of readings for all tests. Such field replicates give an indication of how much variability there is in the equipment, sampling techniques, and environment. To do this: Repeating measurements below or near water-quality standards thresholds: If your measurements at any site are near or beyond the exceedance threshold for state water-quality standards, it’s a good idea to do a replicate to confirm the possible “red-flag” reading. These replicates should agree with the samples within the “Acceptable Differences” in the table above, but the closer the better. Below is a table listing generalized water-quality standards for parameters that have been set by 1. Assign a number to each of your team’s sites that you’re sure you’ll get to. 2. Roll the die in your field kit “Treasure Box” until one of those numbers comes up. Field Procedures Acceptable difference 15 Revised 1/15/2014 WATER CHEMISTRY—GENERAL GUIDELINES the state (ignoring a variety of exceptions and Alternative water-chemistry procedures for poor conditions: If the weather is severe and you wish to minimize your time on the creek, here are a few ideas. In each case, note your deviations from standard procedure on your data sheet. • Calibrate the YSI-60, YSI-85, and turbidimeter at home, and just keep them on throughout your monitoring day, so no warm-up will be needed at each site. (For dissolved oxygen, record the pressure at calibration and at each site.) • pH meter calibration post-checks can be done in the car. • Turbidity samples can be grabbed and taken to your car for readings; just keep the bottle wrapped well to minimize warming, and take readings as soon as possible. Note both collection and reading times. Extra bottles and a plastic tub are in the field kit. • You may also take samples for the other parameters to the car if it’s not too far away: first take a temperature reading in the stream with the YSI-85 (no calibration necessary). Then fill both the regular sampling bottle and the plastic tub, filling completely and closing the lids under water if possible. In transit, be careful not to agitate the tub. (These measures will help to avoid entraining more oxygen into the water.) Take DO readings within 10 min. or they will be flagged “estimated”. In the tub, perform the DO/temp/cond test (moving the probe back and forth at 1 ft/sec), followed by the pH test. Then use the sample bottle for the turbidity tests. In addition to the usual data, note the alternate sampling procedure, actual stream temperature, and both the sample collection and sample reading times on your data sheet. • You may also collect samples for turbidity and pH and take them home; pH should be tested within 2 hours, and turbidity samples can be held 48 hours on ice. • These are contingency measures for poor conditions; use standard protocols if possible, because data collected using these alternative measures may have to be flagged as “estimated” or “rejected”. conditions): Parameters &Water-Quality Exceedances Temperature: > 16° C pH: > 8.5 or < 6.5 pH Turbidity: >5 NTU higher than any upstream site on the same stream, or 10% higher if the upstream turbidity is >50. (As a general rule, take a turbidity replicate if you’re at a downstream site, the turbidity is ≥10, and you’ll be visiting an upstream site on the same day. If the upstream value exceeds the threshold, take a replicate there too.) Dissolved Oxygen: < 9.5 mg/L In the case of dissolved oxygen, the field readings must be corrected for pressure in the following manner: DOcorrected = DOfield X Pressure/29.92 At a high-elevation site on a low-pressure day, the corrected reading could be 10% lower than the field reading; so if the pressure is low and the DO field reading is near the threshold, calculate the corrected reading. (And you can do the same if the field reading is below the threshold but the pressure is high.) If the sample and replicate straddle the threshold, take a third reading and a mean will be calculated. If you’re doing all the water-chemistry procedures yourself, the following is an efficient order in which to perform steps: 1. 2. 3. 4. 5. 6. 7. Check, turn on, and soak the YSI-85. Check and warm up the turbidimeter. Check, turn on, and soak the YSI-60. Hang the air thermometer. Put the YSI-85 in the calibration sleeve. Read the air thermometer. Take the water sample and do turbidity readings. 8. Calibrate the YSI-85 for dissolved oxygen and take readings with it in the stream. 9. Take pH readings with the YSI-60 in the stream. 10. Do post-check of DO drift &pH calibration. 11. Do replicates if needed. Field Procedures 16 15th Edition, 2013 AIR TEMPERATURE EQUIPMENT NEEDED COMMON SENSE AND EXPECTED RANGES: Before packing up, make sure that your air temperature reading conforms to your common sense. As a guide, here’s a chart comparing Celsius degrees (the ones on your thermometer) with Fahrenheit degrees (which Americans are more familiar with). Celsius degrees Fahrenheit degrees 0 32 4 40 10 50 16 60 21 70 27 80 1. pocket stick thermometer 2. data sheet, clipboard, pencil PROCEDURE One person can perform this test. HANGING THE THERMOMETER Unscrew the protective metal tube and put it in your pocket. The thermometer will still be attached to its “hat” in which a string is looped. Make sure the thermometer is dry, and then hang it in a shady spot on the bank with good air circulation, preferably at about eye height, for several minutes to let it stabilize. We suggest you hang the thermometer as soon as you get to your site and then read it later while you’re waiting for some of the other equipment to warm up or stabilize; just don’t leave it hanging in the woods! MEASURING AIR-TEMPERATURE After the thermometer has been hanging for a few minutes, first make sure the sun hasn’t been shining on it. Estimate the reading to the nearest whole degree Celsius (°C) or to more decimals if you can. Wait 30 seconds and estimate again. If the reading hasn’t changed, record it and sampler’s initials on your data sheet. If the reading has changed, jot down the second reading, leave the thermometer hanging, and read it again a few minutes later. Record the temperature once readings have stabilized. Record the time and sampler’s initials. This should be someone who has been properly trained. Screw the metal protective tube back on and put the thermometer back in the treasure box. Replicates not needed for air temperature readings. Field Procedures 17 Revised 1/15/2014 (This page is intentionally blank for printing.) Field Procedures 18 15th Edition, 2013 TURBIDIMETER: HF-DRT 15CE see “If Turbidimeter battery is too low” instructions at the end of this protocol. EQUIPMENT NEEDED Note: Don’t leave this equipment out in freezing temperatures unless you’re using it. If air temperatures are just below freezing, keep the turbidity standards in your pocket—you must keep them from freezing. If the air temperature is below 32°F (0°C), it’s too cold to perform the turbidity procedures in the field—see “Alternative Water-Chemistry Procedures for Poor Conditions”. • • • • • • • • • • • COLLECTING A WATER SAMPLE 1. Don’t sample upstream of where your team will be taking other water-chemistry readings. Communication is key. 2. Enter the stream downstream of where you plan to sample, to avoid contaminating the sample from your boots or stirred-up Tarp HF-DRT 15CE turbidimeter with vials for “zero” & “ten” solutions, plus empty vial (instructions for the 15C meter are similar) watch with second hand or stopwatch sample collection bottle with screw top squirt bottle of purified water small spray bottle of glass-cleaning solution box of lint-free tissues data sheet, clipboard, pencil extra sample bottles or watertight tubs car cigarette-lighter adapter A/C transformer/battery charger sediment. Sample at a point where the stream is flowing and well mixed. (If there is no such place in your normal site area, you may go upstream or downstream, but don’t pass any inflows or outflows, and note your location on the tracking sheet.) Get as far away from the banks as you can. Choose a spot that appears undisturbed. (See Figure 1.) 3. Unscrew the bottle cap, avoiding touching the inside of the cap or the threads. Rinse both the bottle and cap three times in the stream, facing upstream, at a place where your team has not disturbed the bottom-preferably the same spot at which you’re going to collect the sample. When pouring off the rinse water, empty the bottle downstream, so as not to stir up the bottom in the sampling area. 4. If you’re in water >6” deep, hold the bottle near its base and plunge it below the water surface with the opening pointing downward. Collect the sample midway between the bottom and the surface, or 812” below the surface if the water is deep. Turn the bottle underwater into the current What you’re sampling: The turbidity (cloudiness) of the water, measured in Nephelometric Turbidity Units (NTU). High turbidities indicate high concentrations of suspended sediment, which can cause problems for fish and other biota. Where to sample: In this procedure, sampling consists of filling a sample bottle and then performing tests on water from that bottle. Pick an area where the stream is flowing and appears to be well mixed. Do not sample downstream of where your team has disturbed the bottom. INITIAL INSTRUMENT PREPARATION 1. The meter is water-resistant but not waterproof. If it’s raining, close the cover or cover the unit with your body. 2. Turn the meter on to the lowest range to begin its 15-minute warm-up. If the screen reads “BAT,” you must recharge the instrument or plug it into an outlet to use it; Field Procedures 19 Revised 1/15/2014 TURBIDIMETER: HF-DRT 15CE and away from you (see Figure 2). In slowmoving stream reaches, push the bottle underneath the surface and away from you in an upstream direction. Collect at least a pint in the sample bottle, and then cap it under water if possible. In any case, recap the bottle carefully, without touching the inside. b) If there is a drop-off somewhere, as from a cascade or culvert, you can sample from this drop-off so long as the bottle touches nothing but the falling water. TURBIDITY MEASUREMENT Handling the vials: Inside the meter will be one sample vial and two reference vials—one marked on the cap with a number near zero, and the other at some higher number of NTU. Figure 2: Collection procedure when bottle can be submerged 1. Do not ever open the reference vials or unscrew their caps. 2. Take care not to scratch or get dirt on any of the vials. Do not put them down anywhere except inside the meter case. 3. When moving closed vials, hold by the caps only. When opening, closing, or sampling, hold the glass portion of the vials in the area just below the neck, which is outside of their critical measuring area (see diagram below). When possible, hold the vial with a lint-free tissue. 8 5. If the water is <6” deep, you have a couple of options: a) Sample in shallow, fast-moving water, preferably at a point where the water is forced between a couple of larger rocks. Hold the bottle facing upstream so as to catch the moving water in it. Avoid touching the bottom. Field Procedures Taking the readings (with meter still on after the warm-up period): 1. Last calibration date: The latest fullrange calibration date should be marked on a sticker on the face of the meter. Record it on your data sheet only if you’re NOT submitting your data to Clallam County. 20 15th Edition, 2013 TURBIDIMETER: HF-DRT 15CE 2. Zero the meter: Take the ~zero NTU sealed reference vial out of the trough, holding by the cap or upper part only. Clean the critical measuring area with cleaning solution and a lint-free tissue. Place this vial in the meter-well, aligning the arrow on the cap with the white line in the 6:00 position on the well collar. (The meter should still be turned to the lowest range.) Then adjust the REFERENCE ADJUST until the display reads the same as whatever the vial cap is marked as. 3. Check calibration: Take the ~10 NTU sealed reference vial out of the trough, holding by the cap or upper part only. In the space marked “Field Calibration Check,” record the # of NTUs listed on the vial and its expiration date. Clean the critical measuring area with cleaning solution and a lint-free tissue. Place this vial in the meterwell, aligning the arrow on the cap with the white line in the 6:00 position on the well collar. Keep the meter set to the 10-range, even if you see the up-arrow. Record the meter reading to the nearest 0.01 NTU. 4. Calibration check problems: If the above reading differs from what’s written on the vial by more than 5%, try to improve the reading by cleaning the vial again, warming it if it keeps fogging up, or drying the meter-well if it’s wet. If reading is still more than 5% off, continue with the following steps—the data you collect may have to be flagged. 5. Fill the sample vial (remember to hold by the upper part only): a) Thoroughly agitate the sample in the collection bottle—but avoid introducing bubbles by shaking. Immediately fill the sample vial 1/4-1/3 full and shake with the cap on loosely. Empty the sample vial. Repeat this rinse. Then agitate the collection bottle and fill the vial to just below the bottom of the threads. Retighten the vial’s cap. b) Holding the sample vial by the cap, spray cleaning solution on the outside of the Field Procedures glass and wipe it dry with a lint-free tissue. 6. Take the readings: a) Gently invert the vial several times to mix—be careful not to create bubbles. b) Quickly insert the sample vial in the meter well, aligning the arrow on the vial’s cap with the white line in the 6:00 position on the well collar. The readings will change rapidly, then probably slow down after a few seconds. Watch the meter for 30 seconds, then record the whole number (or zero) to which the readings tend most closely during those 30 seconds. (For example, you would record “1” if most readings fall between 0.5 and 1.5.) c) If the meter displays “▲~1 .” or a number >1.2, move to the next higher range. If the meter shows a similar display at its highest range, record “>200” for the model 15C or “>1000” for the 15CE. d) Repeat steps 5 & 6 twice more, for a total of three readings. If readings vary greatly, take more readings until you have three that are close (one unit or 10%, whichever is greater). Record these three readings, the sampling time, and the sampler’s initials. Sampler’s Initials Be sure to put all the initials of one sampler taking responsibility for the data; this should be someone who has been properly trained (see “Quality Assurance” protocol). e) If you are collecting replicates at this site, gather another sample in the sample bottle and repeat this procedure; recalibration not needed. Then see the “Water Chemistry—General” protocol to see if your pairs of readings are within the acceptable precision limits, and resample as needed. f) If the battery goes dead while you’re sampling, see the “If the battery is too low” procedure at the end of this protocol. 21 15th Edition, 2013 TURBIDIMETER: HF-DRT 15CE 7. Clean and store: a) Turn off the meter until you get to your next reach. b) Holding the sample vial by the portion just below the neck, rinse it as follows: i) Pour out the sample water. ii) Fill ¼full with purified water. iii) Screw the cap on loosely. iv) Shake upside down. v) Empty the vial, twisting so that water rinses the sides. vi) Repeat this rinsing one more time. vii) Empty the vial and recap it. c) Place the .02 reference vial in the measuring well, and put the empty sample vial in the trough on the right side of the meter, along with the highernumber reference vial. d) Close the meter. e) Empty the plastic sample collection bottle, recap and store. IF THE TURBIDIMETER BATTERY IS TOO LOW TO USE IN THE FIELD: 1. You can take your sample to the car, plug the adapter included in your kit into the car’s cigarette lighter, and plug the other end into the turbidimeter’s power port on the left side of the vials-trough nearest to the front. (Take out or depress the foam to see it.) Then run your tests. 2. You can collect samples in clean jars, at least pint-sized. If you’re taking replicates, it’s best to take 3 sample bottles from that site, in case the first replicate doesn’t match. (Extra sample bottles are in the dirty bag.) Using duct tape, label them with the site and time of collection. If possible, keep samples on ice and in the dark. Then at the end of the day, bring samples and meter home, plug in the meter using the A/C adapter, and take readings as you would in the field, while the meter is charging (see charging directions below). Samples can be held 48 hours if kept below 4°C (40°F) in the dark; otherwise, the data will be flagged as an “estimate”. If samples are iced, you can let them return to room temperature (in air or a lukewarm bath) to avoid condensation on cold sample vials. On the data sheet, record collection and reading times, as well as holding temperatures and light-exposure. Then continue to charge the meter so you or some other team won’t have trouble the next time! ALTERNATIVE PROCEDURE FOR POOR CONDITIONS: If the weather is severe and you wish to minimize your time on the creek, you may warm up the turbidimeter at home and do the zeroing and calibration check there, and just keep it on throughout your monitoring day and do a final calibration check at the end of the day. Or you may take turbidity samples to your car or home—see next section. Field Procedures TURBIDIMETER BATTERY CHARGERS are in marked zip-lock bags in the field kit “clean bags”; the power port is the front hole on the left side of the vials-trough (take out the vials and foam to see it). The unit does not need to be fully discharged before charging. Turn the meter on, then connect the charger by first plugging it into the meter and then the wall; you should see a “~” in the upper-left of the window. Then you can turn the meter off and let it charge. A full charge takes up to 12 hours but it is okay to partially recharge it. The fully charged meter should be good for at least 5 hours of continuous operation. 22 15th Edition, 2013 TURBIDIMETER: HACH 2100P EQUIPMENT NEEDED Note: Streamkeepers don’t generally take this meter into the field, but instead collect samples and bring them back to the home/office for analysis. Don’t leave this equipment out in freezing temperatures unless you’re using it. If air temperatures are just below freezing, keep the turbidity standards in your pocket—you must keep them from freezing. If the air temperature is below 32°F (0°C), it’s too cold to perform the turbidity procedures in the field—see “Alternative Water-Chemistry Procedures for Poor Conditions”. • • • • • • • • • • • • COLLECTING A WATER SAMPLE 1. Samples can be collected in any clean container, ≥100 mL. 2. Don’t sample upstream of where your team will be taking other water-chemistry readings. Communication is key. Tarp Hach turbidimeter with set of 4 field standards (Blank, low, medium, high), plus empty vial sample collection bottle with screw top squirt bottle of purified water small spray bottle of glass-cleaning solution small bottle of cleaning oil microfiber cloth lint-free tissues data sheet, clipboard, pencil extra sample bottles or watertight tubs car cigarette-lighter adapter A/C transformer/battery charger 3. Enter the stream downstream of where you plan to sample, to avoid contaminating the sample from your boots or stirred-up sediment. Sample at a point where the stream is flowing and well mixed. (If there is no such place in your normal site area, you may go upstream or downstream, but don’t pass any inflows or outflows, and note your location on the tracking sheet.) Get as far away from the banks as you can. Choose a spot that appears undisturbed. (See Figure 1.) 4. If you’re in water >6” deep, hold the bottle near its base and plunge it below the water surface with the opening pointing downward. Collect the sample midway between the bottom and the surface, or 812” below the surface if the water is deep. Turn the bottle underwater into the current and away from you (see Figure 2). In slowmoving stream reaches, push the bottle underneath the surface and away from you in an upstream direction. Collect at least a pint in the sample bottle, then cap it under water if possible. In any case, recap the bottle carefully, without touching the inside. What you’re sampling: The turbidity (cloudiness) of the water, measured in Nephelometric Turbidity Units (NTU). High turbidities indicate high concentrations of suspended sediment, which can cause problems for fish and other biota. Where to sample: In this procedure, sampling consists of filling a sample bottle and then performing tests on water from that bottle. Pick an area where the stream is flowing and appears to be well mixed. Do not sample downstream of where your team has disturbed the bottom. Field Procedures 23 Revised 1/15/2014 TURBIDIMETER: HACH 2100P TAKING READINGS Figure 2: Collection procedure when bottle can be submerged 1. If reading samples that were on ice, minimize condensation on sample vials by: a) Sampling in as dry a room as possible. b) Removing turbidity sample jars from chilled coolers and putting in a room temperature, covered container such as a cardboard box, approximately 30 minutes before taking readings. Alternative method: sample jars can be placed in a warm-water bath for 10 minutes or until room temperature is reached. 2. Prepare vials for readings (BOTH Standards & Sample Vials): a) Hold vials by top only—don’t touch below the white diamond mark. b) Apply a drop of oil and wipe lightly all around the vial reading area with the lint-free cloth labeled “OIL”. c) Wipe the vial dry with the clean lint-free cloth labeled “CLEANER”. d) If vial still isn’t spotless, spray glass cleaner and dab (don’t wipe) the vial dry with a clean lint-free tissue, then wipe with the “CLEANER” cloth again. 8 Pre-Sample Field Standards Testing At the beginning and end of the day in which sample readings are taken, you must assess instrument performance by testing the meter with the set of labeled field standards included with the meter. 1. Turn meter on. 2. Select AUTO RNG (auto-range) and SIG AVG (signal average). 3. Record readings for the “Blank” field standard and all of the Gelex field standard vials (low, medium, and high): a) Place vial in sample well. Diamond on vial lines up with notch on well (facing you). b) Close lid. Failure to close lid will require restarting the meter (turn off and then turn back on). 5. If the water is <6” deep, you have a couple of options: a) Sample in shallow, fast-moving water, preferably at a point where the water is forced between a couple of larger rocks. Hold the bottle facing upstream so as to catch the moving water in it. Avoid touching the bottom. b) If there is a drop-off somewhere, as from a cascade or culvert, you can sample from this drop-off so long as the bottle touches nothing but the falling water. 6. Samples taken away from the field must be stored in darkness at ≤ 4°C. Read samples within 48 hours of their collection time. Field Procedures 24 Revised 1/15/2014 TURBIDIMETER: HACH 2100P c) Press READ. The meter will display various things for about 10 seconds while measuring, and then display the final averaged reading. d) Record the final averaged reading for the field standard vial. e) Repeat for all field standards. f) If readings vary from the stated values on the vials by >5%, try to improve the readings by cleaning the vials again, warming them if they’re fogging up, or drying the meter-well if it’s wet. If readings continue to vary by >5%, continue with readings but notify program managers. Post-Sample Field Standards Testing 1. Record readings for all of the field standard vials. c) Place field standard vial in Hach sample well – align diamond. d) Close lid e) Press READ. f) Record the final averaged reading for the field standard vial. g) Repeat for all field standards. 2. Turn Hach 2100P off. ALTERNATIVE PROCEDURE FOR POOR CONDITIONS: If the weather is severe and you wish to minimize your time on the creek, you may warm up the turbidimeter at home and do the zeroing and calibration check there, and just keep it on throughout your monitoring day and do a final calibration check at the end of the day. Or you may take turbidity samples to your car or home—see next section. Taking Sample Readings 1. Mix the sample bottle thoroughly by gently inverting and swirling several times (the “parade wave”) – do not introduce bubbles. If any bubbles are visible, insert rubber stopper with syringe and pull a suction until they are removed. 2. Rinse sample vials 3 times: a) Fill the Hach sample vial immediately ¼ to ½ full, replace cap, invert/swirl and discard. b) Repeat 3 times. 3. Invert/swirl sample bottle again. 4. Fill sample vial immediately to top of diamond or higher. 5. Dab any water from the outside of the vial with a lint-free tissue. 6. If vial isn’t spotless, wipe outside of vial with “CLEANER” cloth. 7. Invert/swirl sample vial & quickly insert it into the sampling well – align diamond. 8. Close lid. 9. Press READ. 10. Record the final averaged reading for the sample vial. 11. Repeat 3 times. TAKE THREE (3) SEPARATE READINGS FROM EACH SAMPLE, pouring fresh sample into a sample vial each time and following the instructions above. Field Procedures 25 Revised 1/15/2014 TURBIDIMETER: HACH 2100P (This page is intentionally blank for printing.) Field Procedures 26 Revised 1/15/2014 pH: YSI 60 The pH meter needs to be calibrated at the beginning of each day of sampling. The team leader or designee should ideally perform this calibration at home; this can be done several hours prior to leaving for the field. The closer to stream temperature, the better, so you might want to soak or refrigerate the buffer bottles beforehand. A minimum 2-point calibration is necessary, with the two points bracketing the pH values of the sites you’ll be sampling. In the vast majority of circumstances on the North Olympic Peninsula, pH will be between 7 & 10, so these two calibration standards are generally used. In the unusual circumstance that you’ll be sampling where you suspect pH will be 6.5 or lower, you will need to do a 3-point calibration at pH 4, 7 & 10. We have included instructions for 3-point calibration in brackets; you’ll need to get pH 4 buffer from the office, because it won’t normally be stocked in the field kit. EQUIPMENT NEEDED for details). If the probe is in the transport chamber in the meter, simply remove it from this chamber. Check and tighten all connections along the cable, probe, and guard-piece at the end of the probe. Examine the probe. The glass bulb should be intact and clean. 3. Rinse the entire probe with purified water, then carefully dry it with a lint-free tissue, saving the tissue for later. (Or rinse it with some of the extra buffer solution). 4. Place the tall pH 7 buffer bottle in the foam holder, uncap it, insert the probe about 1” into the buffer, shake away any bubbles near the glass sensor, then insert the probe all the way down into this bottle, making sure that the temperature sensor is covered by the solution (see diagram below). If topping up is needed, keep the probe in the buffer and pour against the top part of the probe using the pH 7 refill bottle. Let the probe sit in this solution to stabilize. Meanwhile, on the data sheet for the first site you’ll be visiting later that day, record the Meter’s kit # or name, time, initials, and expiration dates on the pH 7 &10 bottles. Note: Don’t leave this equipment out in freezing temperatures unless you’re using it. If the air temperature is below 23°F (5°C), the YSI meter won’t operate properly and your teammates probably won’t either! • • • • • • • • • • • • Tarp YSI-60 pH meter (probe may be in pH4 buffer solution storage bottle) pH [4,] 7 and 10 buffering solution in high, narrow bottles extra buffer solution for top-up splash-proof goggles & gloves (recommended since buffer contact with skin or eyes can cause irritation) foam holder for pH test bottles watch with second hand or stopwatch bottle of purified water lint-free tissues 6 extra AA alkaline batteries data sheet, clipboard, pencil [plastic tub with tight-fitting lid] CALIBRATION (BEGINNING OF DAY) 1. Turn the instrument on. The instrument will activate all segments of the display for a few seconds, which will be followed by a self test procedure which will last for several more seconds. (If “LO BAT” is displayed or the meter locks up, replace the batteries.) The meter should display pH and °C. If not, press “MODE” until you get to the right display on the screen. 2. If the probe is in the long-term storage bottle, remove it, cap the bottle, and rinse the probe with purified water (see last page Field Procedures 27 Revised 1/15/2014 pH YSI 60 5. Wait for the pH reading to stabilize—not varying by more than 0.01 for 2 min. If the meter still isn’t stable after 10 min., see the “Troubleshooting” section below. 6. Record the “Pre-Cal” temperature (to the nearest tenth) and pH reading (to the nearest hundredth) in the “pH7 pre-cal” section of the data sheet. 7. To enter the calibration menu, simultaneously press both the “UP ARROW” and “DOWN ARROW” keys. The display will show “CAL” at the bottom, “STAND” will be flashing and the main display will show 7.00 (the pH of the first buffer you are using). main screen. “SLOPE” will now appear on the display and be flashing. This indicates that the slope is ready to be set using the second pH buffer. Take the probe out of the pH 7 buffer solution and cap the bottle. 9. Setting the upper point: a) Rinse the entire probe with purified water, then carefully dry the probe. Place the tall pH 10 buffer bottle in the foam holder, uncap it, insert the probe about 1” into the buffer, shake away any bubbles near the glass sensor, then insert the probe all the way down into this bottle, making sure that the temperature sensor is covered by the solution (see prior diagram). If topping up is needed, keep the probe in the buffer and pour against the top part of the probe using the pH 10 refill bottle. Let the probe sit in this solution to stabilize—not varying by more than 0.01 for 2 min. b) Press “ENTER.” The screen will now show “CAL” at the bottom, “SLOPE” will stop flashing, and the pH value for the pH 10 buffer is shown with the right decimal point flashing (see diagram). [Note: The meter automatically accounts for the fact that the true pH of the buffers changes with temperature; therefore, the pH values displayed during calibration won’t always display the same values as what’s written on the buffer bottles. For a table showing how pH buffer differs with temperature, see the table at the end of this protocol.] 8. Setting the midpoint: a) Press the “ENTER” key. The screen will show “CAL” at the bottom, “STAND” will stop flashing and the pH calibration c) When the reading is stable, the decimal point will stop flashing. Press and hold “ENTER” until “SAVE” flashes on the display along with “SLP” to indicate the second slope value has been saved. value is shown with the middle decimal point flashing. b) When the meter decides the reading is stable, the decimal point will stop flashing. Press and hold the “ENTER” key until “SAVE” along with “OFS” is displayed and the display returns to the Field Procedures 28 Revised 1/15/2014 pH YSI 60 f. On your data sheet, record the “post-cal” temperature (to the nearest tenth) and pH (to the nearest hundredth). g. Then record the expected pH reading for that temperature from the graph on the back of your data sheet or the temperature table at end of this protocol, extrapolating as appropriate. h. Next, record the absolute value of the difference between the actual and expected readings; if this is ≤ 0.10 pH unit, you can write “Yes” in the final column, and you’re done. If not, you’ll have to try recalibrating; otherwise, all of your pH data from that day may be flagged as “Estimated” or “Rejected”. i. Rinse the entire probe with purified water and replace it in the meter’s storage chamber (no need to dry). j. You can now turn off your meter until you get to your first site. [The next step is for special low-pH situations only—see introduction to this protocol. For normal situations, you’ll skip this step and go to the next one, “Completing & testing calibration”.] 10. Setting the lower point: a) Rinse the entire probe with purified water, then carefully dry it. Place the tall pH 4 buffer bottle in the foam holder, uncap it, insert the probe about 1” into the buffer, shake away any bubbles near the glass sensor, then insert the probe all the way down into this bottle, making sure that the temperature sensor is covered by the solution (see prior diagram). If topping up is needed, keep the probe in the buffer and pour against the top part of the probe using the pH 4 refill bottle. Let the probe sit in this solution to stabilize—not varying by more than 0.01 for 2 min. b) Press “ENTER.” The screen will now show “CAL” at the bottom, “SLOPE” will stop flashing, and the pH 4 buffer value is shown with the left decimal point flashing. c) When the reading stabilizes, the decimal point will stop flashing. Press and hold “ENTER” to save the first slope until “SAVE” is displayed along with “SLP,” and you return to a normal screen. Calibration troubleshooting: If display reads “undr” or “OVEr” while calibrating, try letting it sit for a few minutes to see if the problem goes away. Also make sure that both the pH and temperature sensors are fully immersed, and try jiggling or shaking the probe in the buffer to dislodge any bubbles that might be sticking to it. If readings do not stabilize after 20-30 minutes, the probe may need cleaning or replacing. Let program managers know about the problem as soon as possible, and if possible, borrow another meter. 11. Completing & testing calibration: a. Press the “MODE” button to return to a normal screen and complete the calibration process. The meter is now calibrated at 2 [or 3] points. b. Take out the probe and cap the buffer bottle. c. Rinse the entire probe with purified water and dry carefully. d. Re-immerse the probe into the pH 7 buffer bottle, following instructions above. e. Wait for the pH reading to stabilize—not varying by more than 0.01 for 2 min. Field Procedures 29 Revised 1/15/2014 pH YSI 60 TAKING READINGS AT SITES “MODE” repeatedly until this screen appears. 2. Place the probe in the water at the spot where you wish to sample, shaking gently to remove any bubbles trapped around the pH sensor. Make sure the pH sensor at the end of the probe and the temperature sensor near the top of the probe are both immersed in a well-mixed part of the stream where the bottom has not been disturbed. You can either: Where to sample: Pick an area where the stream is flowing and appears to be well mixed. Do not sample downstream of where your team has disturbed the bottom. INITIAL INSTRUMENT PREPARATION: 1. If you haven’t already calibrated the meter for the day, do that now (see “Calibration” section at the beginning of this protocol). If you have calibrated already, indicate “Yes” at the top of the data sheet and give the site name of the form on which you recorded the calibration information (this will generally be the first site of the day). 2. If the probe is inside a bottle rather than inside the meter’s chamber, see the “Removing the Buffer Bottle” section at the end of this chapter. 3. Turn on the meter. All segments of the display will be activated for a few seconds. Eventually, pH and temperature will be displayed. If “LO BAT” is displayed, you will need to replace the batteries. If pH and temperature are not displayed, press “MODE” until you get to the right display on the screen. 4. Take the probe out of its chamber. (If it won’t come straight out, turn it slightly clockwise as you pull.) Check the glass bulb and tighten all connections along the cable, probe, and guard-piece at the end of the probe. Find a safe place in the stream to place it for a warm-up. Put it: • downstream of where you will eventually sample (see sampling procedure later in this section); • in a place where the water isn’t too turbulent; • where the bottom isn’t silty or muddy (between a couple of rocks would work); and • where you can safely place the main part of the meter up on the bank. Be sure to shake the probe gently to remove any trapped air bubbles around the pH sensor as you insert it in the water! Dangle the probe at mid-depth in a wellmoving but non-bubbly part of the stream; or • Find a well-mixed pool and swing the probe back and forth at mid-depth; or • In shallow water, wedge the probe between rocks in the middle of a riffle or the tailout of a pool, where the water is moving well. 3. Read the meter to the nearest hundredth of a pH unit. (But do not record it yet.) 4. Wait 2 minutes and read the meter again. a) If the reading has not changed by more than 0.01 pH unit, record that reading to the nearest tenth (not hundredth) on your data sheet. (NOTE: Keep in mind Streamkeepers’ special rounding convention—see “Quality Assurance.”) b) If the reading has changed by more than 0.01 unit, wait another two minutes and try again. Repeat as needed until you’ve met the above criterion. (If you have to pH MEASUREMENT 1. After the YSI-60 pH meter has warmed up in the water, get a screen that shows pH and temperature. You may need to press Field Procedures • 30 Revised 1/15/2014 pH YSI 60 5. 6. 7. 8. wait more than 10 min. to get a stable reading, note that problem on the field sheet and notify program managers.) c) Record the time of sampling and sampler’s initials. If you are collecting replicates at this site, follow this procedure to take another pH reading; recalibration not needed. Then see the “Water Chemistry—General” protocol to see if your pairs of readings are within the acceptable precision limits, and resample as needed. If your reading was 6.5 or lower, AND… • You are NOT reporting your data to Clallam County, AND… • You did not perform a 3-point calibration at the beginning of the day… …then record on your data sheet the last 3point calibration date, written on a sticker on the side of the meter. A later check of the meter will confirm the lower point. Shake off the probe, rinse with purified water, and pat it dry with lint-free tissues. Meter calibration post-check: d) Once the meter has stabilized, record the “pH meter post-check” temperature (to tenths) and pH (to hundredths). e) Record the expected buffer value from the temperature-correction graph on the back of the data sheet or the chart below. Extrapolate as appropriate from the values in that chart. f) Record the absolute value of the difference between the actual and expected readings; if this is ≤ 0.10 pH units, you can write “Yes” in the last column, and you’re done. If not, you’ll have to try recalibrating the meter (using the procedure at the beginning of this section) and then re-doing the readings; otherwise, the pH data you just took (as well as probably all subsequent data you take that day) will be labeled “Estimated” or “Rejected”. 9. Rinse with purified water, reinsert into the chamber, and turn off the meter. ALTERNATIVE WATER-CHEMISTRY PROCEDURES FOR POOR CONDITIONS: See “Water Chemistry—General Guidelines” protocol. NOTE: It would be adequate to just perform this post-test at the end of each day; however, if the meter fails that test, all data from that day would be invalid. The only way to assure acceptable data is to perform the post-test at each site, and then re-calibrate if the meter fails that test. Generalized pH Buffer Values at Various Temperatures (from BDH buffers 2009) Temperature pH 4 pH 7 pH 10 0°C 4.00 7.12 10.31 5°C 4.00 7.09 10.23 10°C 4.00 7.06 10.17 15°C 4.00 7.04 10.11 20°C 4.00 7.02 10.05 25°C 4.00 7.00 10.00 30°C 4.01 6.99 9.95 35°C 4.02 6.98 9.91 a) Immerse the dried probe all the way into the pH 7 buffer test bottle, using the foam bottle holder to stabilize it. The temperature sensor (see diagram) must be immersed in the buffer—top up as needed from the extra pH 7 bottle. If it’s raining, cover the buffer bottles with your body. Also, if possible, have a second person assist you by holding caps and screwing them right back on when finished with them. Keep the lids of these bottles screwed on tight when not in use. b) Record the time and sampler’s initials. c) Wait for the pH reading to stabilize (not varying by more than 0.01 for 2 min.). Field Procedures (Actual values will vary from product to product, but these should be close enough to check instrument calibration.) 31 Revised 1/15/2014 pH YSI 60 Removing the buffer bottle from the pH 6. 7. 8. 9. Velcro cap with buffer probe Don’t unscrew this end piece! Velcro O-ring under cap Switch these caps when you remove the bottle from the both caps, and O-ring are all stored together in a single “package” (see drawing below). Wrap this “package” in a small Ziploc bag and store in the treasure box. Move the tape that’s covering the probe chamber to the side of the meter, being careful not to lose the little sponge that’s inside. Add a few drops of purified water to the little sponge inside the chamber. If possible, soak the probe in creek water for 30 minutes before taking your first reading. If you know that the meter won’t be used for a few days, store the probe back in the buffer-solution bottle (see first diagram), wrap the Ziploc bag around it, and close it as far as possible to help keep it intact. Recover the probe chamber hole with the tape to keep the sponge from falling out. closed probe (YSI-60) We store the pH probe in pH4 buffer solution to keep it in good shape if it’s not going to be used for a week or more. Sometimes we may neglect to take the probe out of this bottle before we send out the kit. If this happens: 1. Remove the “closed cap” from the Velcro at the bottom of the bottle. 2. Holding the bottle upright, unscrew it from the cap with the hole (“open cap”) and screw the closed cap onto it. 3. Rinse the probe and open cap with purified water. 4. Slide the open cap toward the cord to expose the O-ring beneath the cap. Roll off the O-ring, then slide the open cap off the end of the probe. 5. Sandwich the O-ring between the Velcro on the bottom and the Velcro on the open cap, so that it doesn’t fall out. Thus, the bottle, Field Procedures 32 Revised 1/15/2014 MULTIMETER: YSI-85 sheet, stuff a lint-free tissue inside, and wet it with a few drops. 4. Check and tighten all connections along the cable, probe, and guard-piece at the end of the probe. Examine the probe. All holes should be clean of debris, and the gold cathode on the end should be shiny. The plastic membrane over the cathode should not be loose, wrinkled, or damaged, and there should be no bubbles under it. Rinse if dirty. Note any unsolvable problems on your data sheet and continue if possible with the procedure. 5. Place the probe in the stream. Set the meter in a safe place on the bank for 15 minutes to let the meter warm up and the probe stabilize to stream temperature. 6. Record the barometric pressure, to the nearest 0.01 in Hg (inches of mercury), plus time and sampler’s initials. If the screen does not read “BARO” in the upper-left corner, hit the MODE button until it does. If it does not say “inHg” in the upper-right corner, hit the RESET button until it does. EQUIPMENT NEEDED Note: Don’t leave this equipment out in freezing temperatures unless you’re using it. If the air temperature is below 23°F (5°C), the YSI meter won’t operate properly and your teammates probably won’t either! • • • • • • YSI-85 multimeter Open-cell foam probe calibration sleeve Brunton ADC Summit pocket barometer watch with second hand or stopwatch 6 extra AA alkaline batteries data sheet, clipboard, pencil Where to sample: Pick an area where the stream is flowing and appears to be well mixed. Do not sample downstream of where your team has disturbed the bottom. INITIAL INSTRUMENT PREPARATION: 1. Turn on the meter. The instrument will activate all segments of the display for a few seconds, then go through a self-test procedure that will last a few more seconds. A number will be displayed, along with the letters “CEL.” That number should be between 4.8-5.2. If not, report the number on the data sheet and to the office staff. 2. If the unit displays “Err” at this point, and “Err” does not disappear after a few seconds, try turning the unit off and back on again. If it displays “LO BAT,” replace the batteries and discard the old ones. If it displays other error messages, you will not be able to use the instrument—record the problem and let the staff know about it as soon as possible. If it displays number readings, “rcl,” or “ErAS,” the meter is functioning properly. 3. Remove the probe from the meter’s chamber. Turn the chamber upside down. If the sponge inside is dry and falls out, reinsert it and wet it with a few drops of water, noting that it was dry on your data sheet. If it’s missing, note that on your data Field Procedures If you have to change the barometer battery in the field, you’ll have to reset the meter’s “Offset” value before taking readings: 33 • Press the Mode button until Baro inHG shows at top of screen • If not in inHG mode, press Reset to cycle through choices until inHG shows. • Press and hold the Mode button until Storm Off shows. • Release the Mode button and press it again one time. • Now you should see Offset: and a decimal number. • Press and hold Reset until the decimal number begins to flash, then release the button. • The proper Offset value should be written on a sticker on the back of the barometer. Press Reset (increases value) or Set (decreases value) until this proper Offset value shows. • Press Mode once to exit set mode - value stops flashing. • Press and hold Mode button until you only see Baro inHG and the barometric pressure. Revised 1/15/2014 MULTIMETER_DO-TEMP-COND-SAL TAKING MEASUREMENTS FOR DISSOLVED OXYGEN, TEMPERATURE, CONDUCTIVITY, AND SALINITY: use the UP or DOWN ARROW buttons to make it zero. Then press ENTER.NOTE: If you don’t have a barometer and won’t be able to get a pressure reading later (e.g., from a nearby weather station), then you should enter the altitude to the nearest number of hundreds of feet. For instance, if you’re at 800 feet, you’d enter “8”. (Elevations of your sites should be on your forms folder.) On your data sheet, explain what you’ve done and why. BUTTON BUMMERS: The YSI-85’s buttons are slow to respond, so wait a few seconds after pressing any button to give the meter time to react. Otherwise, you may skip over the screen you want. Also, sometimes the buttons don’t respond at all and you have to try again. Just be patient. 1. Calibrate the meter for dissolved oxygen: a) Take the foam calibration sleeve out of its bag and wet it in the stream, then gently wring it out. Take the probe out of the stream where it’s been soaking, rinse off any dirt, and firmly flick water off the probe as if you were shaking down a fever thermometer. Place the probe into the foam sleeve, pulling the probe back about ½” from the end to keep any foam from touching the DO membrane. b) Put the meter and probe in a safe spot, preferably out of the sun. If it’s near freezing, set the sponge on the tarp – it will stick to frozen rocks. c) Erase prior readings from the meter: • Press the MODE button as many times as needed for “ErAS” to appear on the screen. • Press the DOWN ARROW and ENTER buttons simultaneously for approximately 5 seconds. • When “DONE” flashes on the screen for 1-2 seconds, the data have been erased, and the meter will automatically return to normal operation (DO % Saturation screen). d) Wait for stabilization of the probe inside the calibration sleeve, defined as follows: STABILIZATION CRITERION: During a period of 2 minutes, both DO Sat % and temp (°C) stay within 0.1 of their initial readings. f) The meter will now show CAL & 100.0 in the lower part of the display. Confirm stabilization for another 30 seconds. TROUBLESHOOTING THE DO METER: If the meters don’t stabilize within 10 minutes of observation, try each of these steps in the following order, trying again to stabilize after each step: • Take the probe out of the sleeve, squeeze out any excess water, and shake off the probe. Turn the meter off and then on. • Turn off the meter, take out the batteries, wipe them and the inside of the battery cover-plate with a cloth, and re-insert them in a different order (but according to the diagram on the inside of the tubes). • Try the above step again. Yep, again! • Replace the batteries with the fresh batteries in the “Treasure Box” of your kit’s Clean Bag. If problems persist, note on your data sheet the variation in readings within your last stabilization observation period, and proceed. g) When you have confirmed stabilization, press ENTER. The display should show “SAVE” and then a reading near 100%. The instrument is now calibrated for DO. 2. Take the probe out of the calibration sleeve. If there are droplets on the membrane big enough to roll off, shake them off and recalibrate (or your readings will not be accurate). If there are no droplets, you can set the foam sleeve aside. 3. Re-check the barometric pressure, to the nearest 0.01 in Hg (inches of mercury). If not the same as the earlier reading, record this second reading as well. e) When you believe the probe has stabilized, press both UP and DOWN ARROW buttons at the same time. The screen should then read zero; if needed, Field Procedures 34 15th Edition, 2013 MULTIMETER_DO-TEMP-COND-SAL 4. Insert the probe in the stream: Standing downstream or to the side of the probe, hold it in the current, facing the probe upstream, in a place with steady flow, adequate depth, good mixing, and no surface turbulence. If the current is < 1 ft/sec, hold the probe halfway down in the water column and stir back and forth so that water moves over it at the rate of at least 1 ft/sec; but do not create bubbles. Keep the entire probe below water level—see following diagram. Water level should be at least up to the cable connection— but be careful not to kink the wire at this stress point! any steady rise or fall; and during a 30 second observation, they don’t vary by more than 0.5% DO and 0.1°C. Then press ENTER and hold for 2 seconds. The meter will flash SAVE on the display along with a data-point number (which should be 01 if you erased previous readings). You have now saved readings for all parameters. 6. If you’re taking replicates at this site: Remove probe from stream, shake off water, replace in stream, and collect a second reading (same as above). At “Save,” the data-point number should show as 02. Also take a replicate barometer reading and record it with the replicate data. water level 7. Shake off the probe, rinse with purified water if the stream water is dirty, and replace the probe in its sleeve. Put the unit in the shade if possible. 8. Record the number or name written on the meter (e.g., “1” or “OPI”). And if you are not submitting the data to Clallam County, record the latest calibration dates for DO (“Winkler”), conductivity, and temperature, which should be written on stickers on the meter. 9. Record the sampling time on your data sheet, to the nearest minute. 10. Record the readings: Press MODE repeatedly until “rcl” (recall) is displayed on the screen. The number below “rcl” is the data-point number the meter gave when it saved your data. Use the Up/Down arrows as needed to get to the number you want. (01 should be your sample and 02 your replicate, if you did one.) Then press ENTER successively to record the following readings, in the following order, using our rounding convention as necessary (see Quality Assurance protocol): IN LOW OR SLOW WATER CONDITIONS… • The surface water may be traveling at 1 ft/sec, but just below the surface it may be considerably slower due to the friction of the bottom sediment. Therefore, do not simply take a reading just below the surface in very shallow water. Try to find a little pool in which to stir the probe back and forth without disturbing the bottom. • You can also look for a little riffle in which the water cascades between a couple of rocks, wedging the probe between the rocks with the water flowing over it. If the Flow team is available and the water is deep enough to immerse the propeller, have them come over and measure the velocity at the spot where the DO membrane will be; or hold the probe down in there and try to feel the force of the water. If it seems satisfactory, wedge the probe into the rocks with the conductivitysensor holes facing up and the tip of the probe upstream of any place you’ve touched the rocks. • The best method would be to test for DO using both methods and record the readings with the higher values. a) Temperature: to nearest 0.1°C. b) DO % Saturation: to nearest 0.1%. c) DO Concentration: to nearest 0.1 mg/L. d) Conductivity: You will see a screen with a figure in “µS” or “mS” and the “°C” symbol not flashing. Go to the 5. Stabilize and save the readings: Wait for stabilization according to the following criteria: Both readings have stopped Field Procedures 35 15th Edition, 2013 MULTIMETER_DO-TEMP-COND-SAL next screen, where the “°C” symbol is flashing, indicating that the parameter being measured is temperaturecompensated conductivity. Record to the nearest whole number of µS(microSiemens). (If you go too far, work your way around again.) If the reading is in mS (milliSiemens), multiply by 1000 (i.e., move the decimal place 3 places to the right) to convert to µS, and record to the nearest whole number. e) Salinity: Record the next screen, which shows a “ppt” symbol, to the nearest tenth. This is the salinity in parts per thousand. 11. If you have replicates to transcribe, use the DOWN arrow to get to the proper “rcl” datapoint number (probably 02), then continue as above to record readings. Next, check the “Water Chemistry—General” protocol to see if your pairs of readings are within the acceptable precision limits, and resample as needed. 12. Record the sampler’s initials for both sample and replicate. COMMON SENSE AND EXPECTED RANGES: Please compare your readings with the expected ranges on the datasheet. If you’re outside the expected range, consider resampling or troubleshooting with your fellow samplers. Conductivity readings in particular have a nasty habit of being wacky. Stream conductivity is rarely lower than 25 µS. If your readings are lower than this, you’ll need to troubleshoot: -- If the reading is 0.0 or 0.1, you might be reading the salinity (“ppt”) screen rather than the proper conductivity screen; if so, scroll through the screens again (by pressing ENTER) until you get to the right one. -- You might not have held the probe completely underwater. Try taking another set of readings. -- The readings might be in mS rather than µS (see above). Sampler’s Initials Be sure to put all the initials of one sampler taking responsibility for the data; this should be someone who has been properly trained (see “Quality Assurance” protocol). 13. Perform a DO drift check: Hit the MODE button twice to get back to the real-time DO %Sat screen. Re-wet the calibration sponge in the stream, wring it out gently, and reinsert the probe as before. Keep the meter and probe in the shade, if possible, and allow the probe to stabilize as before: ELECTRONIC PROBLEMS? If the YSI meters stop showing all the decimals, show wacky readings, or don’t respond when you press buttons, try the battery tricks described above. They’ll probably work! If not, note what happened on your data sheet and notify program staff. data will be flagged as “estimated” or “rejected”. 14. If the stabilized DO % Saturation reading is satisfactory, record it to the nearest 0.1%. 15. Record the time and sampler’s initials. 16. Turn off the meter, put the probe into the meter’s chamber, and put the calibration sponge back into its bag. STABILIZATION CRITERION: During a period of 2 minutes, both DO Sat % and temp (°C) stay within 0.1 of their initial readings. Do NOT hit any buttons on the meter. When stabilization is reached, you’ll want the DO % Saturation reading to be between 98-102%; if not, you’ll need to re-calibrate the meter and re-take the readings, or your Field Procedures MEASURED VS. CORRECTED READINGS: The data for DO saturation and concentration will get adjusted once entered into the database, according to the pressure, temperature, and salinity you recorded. This formula avoids a built-in error in the YSI-85, which assumes “normal” atmospheric pressure for a given altitude, when actually that pressure can vary from normal by 5% or more. 36 15th Edition, 2013 MULTIMETER_DO-TEMP-COND-SAL ALTERNATIVE MULTIMETER PROCEDURE FOR POOR CONDITIONS: If the weather is severe and you wish to minimize your time on the creek, you may collect a sample and conduct testing in your car within 10 minutes (see Water Chem—General chapter & Standard Methods 4500-O): • Calibrate the YSI-85 at home, with the soaking sponge as close to stream temperature as possible; note both water temperature and Field Procedures • • 37 barometric pressure. At each site, be sure to warm up the meter for 15’ before taking readings (or just keep it on all day); note barometric pressure at each site. Explain the deviance from normal procedures on your data sheet. Staff will have to adjust your data because of pressure differences between calibration and sampling sites. 15th Edition, 2013 HYDROLAB QUANTA This page is intentionally blank for printing. Field Procedures 38 15th Edition, 2013 MULTIMETER: HYDROLAB QUANTA DO Calibration and Operation NOTE: These instructions presume that the instrument has had the following calibrations/checks performed, preferably the day before—see calibration/check sheets at the end of this protocol: • Calibration for conductivity, pH, and turbidity, per the Hydrolab manual. • Validation of the DO sensor with a side-by-side Winkler titration or other means (see Winkler titration instructions on Streamkeepers’ website under “Quality Assurance”). Overview The control keys are on the device handle; see figure below. Handle the instrument very carefully, as bumps or large temperature changes can change the tension on the membrane and get the instrument out of calibration. You will be doing: 1. pre-sampling calibration, 2. the sampling itself and 3. a post-sampling quality check. The Hydrolab measures the following parameters: • • • • • • Temperature Dissolved oxygen Specific conductivity (25°C) pH Salinity Turbidity Hydrolab Display & Controls The display shows readings of 5 parameters at once, on two screens. A menu bar is located at the bottom of the screen. A figure of the first data screen is shown below. PRE-SAMPLING DISSOLVED OXYGEN CALIBRATION—perform at beginning of sampling day Turn on meter. It will take about 30 seconds for the meter to run through self-checks, then the screen will change to one with ‘Temp’ at the upper left and ‘Screen’ flashing in the middle of the bottom menu bar (see diagram at left). 1. Data Sheet Fill out top part of the Pre/Post Calibration Check data sheet, left-hand column, with date, time and samplers, if it has not already been filled in. (See sample data sheet following this protocol.) Field Procedures 39 15th Edition, 2013 HYDROLAB QUANTA 2. Battery check Hit the Enter key. Check and record the voltage. Generally you should replace the batteries if: • the voltage reads < 3.5V • the display shows dashes instead of digits; or • parts of the display are missing. 3. Remove storage cup Carefully remove the plastic storage cup so it retains the water, and set aside. 4. Check DO membrane Place the black rubber calibration cup cover [concave up] loosely over the top of the calibration cup. Prop the instrument up in a secure spot, without kinking the cable. Hit the Enter key; this will take you to the screen with DO mg/L [Screen 1] and wait for this stabilization criterion to be met: Stabilization has been achieved when the DO mg/L value does not change more than +/- 0.01 mg/L for 2 minutes. When stabilization is achieved, record the pre-calibration DO mg/L reading on the lefthand column of the data sheet, in the DO Calibration section. Also record the temperature reading at stabilization, on the data sheet. 6. Record barometric pressure Record the barometric pressure on your data sheet, from a barometer measuring in mmHg. If your barometer reads in inHg, you must convert to mmHg by multiplying inHg by 25.4. If your barometer reads in mbar, convert to mmHg by multiplying mBar by 0.75. Also record info about the barometer used. 7. Set calibration Navigate to the ‘Calib’ screen, on the menu bar, by using the Left/Right arrow key. Hit Enter. Select DO% with Down arrow, then hit Enter. On the Hydrolab DO calibration screen, adjust barometric pressure, which is flashing, to the value you recorded in mmHg in the section above, by using the Up/Down arrows, then press Enter. Now, hit Esc to return to Screen 1 and record the post-calibration DO mg/L reading on your data sheet. 8. Check calibration Record the ‘expected’ DO mg/L reading from the DO Solubility Chart [see Solubility Chart following this protocol]. Your post-calibration DO should be within 2% of the expected Carefully rotate the black turbidity sensor ring out so you can see the sensors beneath. The DO membrane is the stretched plastic membrane with the black O-ring around the sides. Gently shake all droplets off this membrane. Check the DO sensor’s membrane for wrinkles or bubbles underneath and note on data sheet. Rotate the black turbidity ring back to center. 5. Saturated-air DO reading Attach the plastic cup with an opening at the narrow-end; this is the calibration cup. With the open narrow-end pointing upward, fill with water from the storage cup and top off as needed with room-temp de-ionized water or tap water. Bring the water level up to just below the O-ring, at the base of the DO membrane. It should NOT cover it. Re-check for any droplets on the membrane and remove with tissue or by blowing. Field Procedures 40 15th Edition, 2013 HYDROLAB QUANTA 4. Record or save data Either record data immediately, or: Press the Right arrow one time to navigate to ‘Store’ on the menu bar. Press Enter. The screen will show your data reference number at the bottom. To exit Store mode, press Enter. reading from the Solubility Chart. If not, try re-calibrating. 9. Store probe and meter Turn off the Hydrolab and replace the storage cup in anticipation of sampling. Storage cup should hold approx. 1” of deionized water. 5. Retrieve stored data To recall saved data, use arrow keys to navigate to ‘Review’ on menu bar. Press Enter. Use the arrow keys to recall your data reference number, and record data on data sheet. Note: The screen cycles between two data screens, and you’ll need to pull some of the data you need from each screen. Do not record DO%, as that may not be accurate, depending on barometric pressure. HYDROLAB SAMPLING OPERATION Turn on meter. It will take about 30 seconds for the meter to run through self-checks, then the screen will change to one with ‘Temp’ at the upper left and ‘Screen’ flashing at the bottom center in the menu bar. Hit the Enter key. Check and record the voltage. Generally you should replace the batteries if the voltage reads <3.5V. 1. Install sampling cup Carefully remove the plastic storage cup so it retains the water, and set aside. Replace with the sampling cup—the one with side slots. 2. Warm up / Cool down Place the Hydrolab probe in a safe, clean part of the stream for a 10-minute warm-up/cooldown soak. 3. Sampling Deploy the probe for readings by either: a. Placing the probe in a place with > 1 ft/sec velocity across the membrane1; b. Turning on the Sample Circulator; or c. Waving the sensor back and forth at > 1 ft/sec. 6. Erase data Press Enter. ‘Clear’ and ‘Clear All’ will appear at the bottom of the screen. Use arrow keys to select either. Press Enter to clear the memory. If you want to keep the data press Esc. 7. Store probe and meter Turn off the meter by pressing On/Off button till countdown reaches 0. Remove the sampling cap and replace with the storage cup between sites, keeping the water inside it. POST-SAMPLING CHECK Use the same data sheet you used with the presampling calibration, but fill in the right hand side now. 1. Repeat pre-sampling steps Repeat the pre-sampling steps above, except the “Set Calibration” step, as you are doing a drift check and not re-calibrating. 2. Drift check pass? Determine whether the drift check passed by checking DO mg/L values versus the Solubility Chart DO mg/L values. [See Solubility Chart following this protocol]. Drift check passes if there is ≤ 2% deviation between compared values. Wait for stabilization criteria to be met; during a 30 second observation: • • • Temp should not change by > 0.1° C DO should not change by > 0.05 mg/L pH should not change by > 0.01 1 There must be >1 ft/sec flow across the DO membrane for an accurate reading. One way to test if the flow is adequate is to first note the DO mg/L reading with the probe sitting in the water, and then trying either method (b) or (c) and seeing if the reading increases. Field Procedures 41 15th Edition, 2013 HYDROLAB QUANTA Field Procedures 42 Revised 1/15/2014 HYDROLAB QUANTA Field Procedures 43 15th Edition, 2013 HYDROLAB QUANTA Pressure Conversion Table Millibars In. Hg. Mm Hg. Millibars In. Hg. Mm Hg. Millibars In. Hg. Mm Hg. 900 901 902 903 904 905 906 907 908 909 910 911 912 913 914 915 916 917 918 919 920 921 922 923 924 925 926 927 928 929 930 931 932 933 934 935 936 937 938 939 940 941 942 943 944 945 946 947 948 949 26.58 26.61 26.64 26.67 26.70 26.72 26.75 26.78 26.81 26.84 26.87 26.90 26.93 26.96 26.99 27.02 27.05 27.08 27.11 27.14 27.17 27.20 27.23 27.26 27.29 27.32 27.34 27.37 27.40 27.43 27.46 27.49 27.52 27.55 27.58 27.61 27.64 27.67 27.70 27.73 27.76 27.79 27.82 27.85 27.88 27.91 27.94 27.96 27.99 28.02 675.1 675.8 676.6 677.3 678.1 678.8 679.6 680.3 681.1 681.8 682.6 683.3 684.1 684.8 685.6 686.3 687.1 687.8 688.6 689.3 690.1 690.8 691.6 692.3 693.1 693.8 694.6 695.3 696.1 696.8 697.6 698.3 699.1 699.8 700.6 701.3 702.1 702.8 703.6 704.3 705.1 705.8 706.6 707.3 708.1 708.8 709.6 710.3 711.1 711.8 950 951 952 953 954 955 956 957 958 959 960 961 962 963 964 965 966 967 968 969 970 971 972 973 974 975 976 977 978 979 980 981 982 983 984 985 986 987 988 989 990 991 992 993 994 995 996 997 998 999 28.05 28.08 28.11 28.14 28.17 28.20 28.23 28.26 28.29 28.32 28.35 28.38 28.41 28.44 28.47 28.50 28.53 28.56 28.59 28.61 28.64 28.67 28.70 28.73 28.76 28.79 28.82 28.85 28.88 28.91 28.94 28.97 29.00 29.03 29.06 29.09 29.12 29.15 29.18 29.21 29.23 29.26 29.29 29.32 29.35 29.38 29.41 29.44 29.47 29.50 712.6 713.3 714.1 714.8 715.6 716.3 717.1 717.8 718.6 719.3 720.1 720.8 721.6 722.3 723.1 723.8 724.6 725.3 726.1 726.8 727.6 728.3 729.1 729.8 730.6 731.3 732.1 732.8 733.6 734.3 735.1 735.8 736.6 737.3 738.1 738.8 739.6 740.3 741.1 741.8 742.6 743.3 744.1 744.8 745.6 746.3 747.1 747.8 748.6 749.3 1000 1001 1002 1003 1004 1005 1006 1007 1008 1009 1010 1011 1012 1013 1014 1015 1016 1017 1018 1019 1020 1021 1022 1023 1024 1025 1026 1027 1028 1029 1030 1031 1032 1033 1034 1035 1036 1037 1038 1039 1040 1041 1042 1043 1044 1045 1046 1047 1048 1049 1050 29.53 29.56 29.59 29.62 29.65 29.68 29.71 29.74 29.77 29.80 29.83 29.85 29.88 29.91 29.94 29.97 30.00 30.03 30.06 30.09 30.12 30.15 30.18 30.21 30.24 30.27 30.30 30.33 30.36 30.39 30.42 30.45 30.47 30.50 30.53 30.56 30.59 30.62 30.65 30.68 30.71 30.74 30.77 30.80 30.83 30.86 30.89 30.92 30.95 30.98 31.01 750.1 750.8 751.6 752.3 753.1 753.8 754.6 755.3 756.1 756.8 757.6 758.3 759.1 759.8 760.6 761.3 762.1 762.8 763.6 764.3 765.1 765.8 766.6 767.3 768.1 768.8 769.6 770.3 771.1 771.8 772.6 773.3 774.1 774.8 775.6 776.3 777.1 777.8 778.6 779.3 780.1 780.8 781.6 782.3 783.1 783.8 784.6 785.3 786.1 786.8 787.6 Field Procedures 44 15th Edition, 2013 HYDROLAB QUANTA Solubility of Oxygen in Fresh Water at Various Temperatures and Pressures [Solubility shown in milligrams per liter. Values based on published equations by Benson and Krause (1980 and 1984) °C 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0 5.5 6.0 6.5 7.0 7.5 8.0 8.5 9.0 9.5 10.0 10.5 11.0 11.5 12.0 12.5 13.0 13.5 14.0 14.5 15.0 15.5 16.0 16.5 17.0 17.5 18.0 18.5 19.0 19.5 20.0 20.5 21.0 21.5 22.0 22.5 23.0 23.5 24.0 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 600 11.5 11.4 11.2 11.1 10.9 10.8 10.6 10.5 10.3 10.2 10.1 9.9 9.8 9.7 9.6 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.5 7.4 7.4 7.3 7.2 7.1 7.1 7.0 6.9 6.9 6.8 6.7 6.7 6.6 6.5 6.5 6.4 6.3 6.3 6.2 6.2 6.1 6.1 6.0 6.0 5.9 605 11.6 11.5 11.3 11.1 11.0 10.8 10.7 10.6 10.4 10.3 10.1 10.0 9.9 9.8 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.6 8.5 8.5 8.4 8.3 8.2 8.1 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 6.9 6.8 6.8 6.7 6.7 6.6 6.5 6.5 6.4 6.3 6.3 6.2 6.2 6.1 6.1 6.0 6.0 Field Procedures 610 11.7 11.6 11.4 11.2 11.1 10.9 10.8 10.6 10.5 10.4 10.2 10.1 10.0 9.8 9.7 9.6 9.5 9.4 9.3 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.8 7.7 7.6 7.6 7.5 7.4 7.3 7.3 7.2 7.1 7.0 7.0 6.9 6.8 6.8 6.7 6.6 6.6 6.5 6.5 6.4 6.3 6.3 6.2 6.2 6.1 6.1 6.0 615 11.8 11.7 11.5 11.3 11.2 11.0 10.9 10.7 10.6 10.5 10.3 10.2 10.1 9.9 9.8 9.7 9.6 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.1 8.0 8.0 7.9 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.2 7.2 7.1 7.0 7.0 6.9 6.8 6.8 6.7 6.6 6.6 6.5 6.5 6.4 6.3 6.3 6.2 6.2 6.1 6.1 620 11.9 11.7 11.6 11.4 11.3 11.1 11.0 10.8 10.7 10.5 10.4 10.3 10.1 10.0 9.9 9.8 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.2 7.2 7.1 7.0 7.0 6.9 6.8 6.8 6.7 6.6 6.6 6.5 6.4 6.4 6.3 6.3 6.2 6.2 6.1 625 12.0 11.8 11.7 11.5 11.4 11.2 11.1 10.9 10.8 10.6 10.5 10.3 10.2 10.1 10.0 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.4 8.3 8.2 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.5 7.4 7.4 7.3 7.2 7.1 7.1 7.0 6.9 6.9 6.8 6.7 6.7 6.6 6.6 6.5 6.4 6.4 6.3 6.3 6.2 6.2 630 12.1 11.9 11.8 11.6 11.4 11.3 11.1 11.0 10.8 10.7 10.6 10.4 10.3 10.2 10.0 9.9 9.8 9.7 9.6 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.4 7.4 7.3 7.2 7.1 7.1 7.0 6.9 6.9 6.8 6.7 6.7 6.6 6.6 6.5 6.4 6.4 6.3 6.3 6.2 Barometric Pressure (mm Hg) 635 640 645 650 655 660 12.2 12.3 12.4 12.5 12.6 12.7 12.0 12.1 12.2 12.3 12.4 12.5 11.9 12.0 12.1 12.1 12.2 12.3 11.7 11.8 11.9 12.0 12.1 12.2 11.5 11.6 11.7 11.8 11.9 12.0 11.4 11.5 11.6 11.7 11.7 11.8 11.2 11.3 11.4 11.5 11.6 11.7 11.1 11.2 11.3 11.3 11.4 11.5 10.9 11.0 11.1 11.2 11.3 11.4 10.8 10.9 11.0 11.1 11.1 11.2 10.7 10.7 10.8 10.9 11.0 11.1 10.5 10.6 10.7 10.8 10.9 10.9 10.4 10.5 10.5 10.6 10.7 10.8 10.3 10.3 10.4 10.5 10.6 10.7 10.1 10.2 10.3 10.4 10.4 10.5 10.0 10.1 10.2 10.2 10.3 10.4 9.9 10.0 10.0 10.1 10.2 10.3 9.8 9.8 9.9 10.0 10.1 10.1 9.6 9.7 9.8 9.9 9.9 10.0 9.5 9.6 9.7 9.8 9.8 9.9 9.4 9.5 9.6 9.6 9.7 9.8 9.3 9.4 9.4 9.5 9.6 9.7 9.2 9.3 9.3 9.4 9.5 9.6 9.1 9.2 9.2 9.3 9.4 9.4 9.0 9.1 9.1 9.2 9.3 9.3 8.9 8.9 9.0 9.1 9.2 9.2 8.8 8.8 8.9 9.0 9.1 9.1 8.7 8.8 8.8 8.9 9.0 9.0 8.6 8.7 8.7 8.8 8.9 8.9 8.5 8.6 8.6 8.7 8.8 8.8 8.4 8.5 8.5 8.6 8.7 8.7 8.3 8.4 8.4 8.5 8.6 8.6 8.2 8.3 8.4 8.4 8.5 8.5 8.1 8.2 8.3 8.3 8.4 8.5 8.0 8.1 8.2 8.2 8.3 8.4 8.0 8.0 8.1 8.2 8.2 8.3 7.9 7.9 8.0 8.1 8.1 8.2 7.8 7.9 7.9 8.0 8.0 8.1 7.7 7.8 7.8 7.9 8.0 8.0 7.6 7.7 7.8 7.8 7.9 7.9 7.6 7.6 7.7 7.7 7.8 7.9 7.5 7.5 7.6 7.7 7.7 7.8 7.4 7.5 7.5 7.6 7.7 7.7 7.3 7.4 7.5 7.5 7.6 7.6 7.3 7.3 7.4 7.4 7.5 7.6 7.2 7.3 7.3 7.4 7.4 7.5 7.1 7.2 7.2 7.3 7.4 7.4 7.1 7.1 7.2 7.2 7.3 7.3 7.0 7.0 7.1 7.2 7.2 7.3 6.9 7.0 7.0 7.1 7.2 7.2 6.9 6.9 7.0 7.0 7.1 7.1 6.8 6.9 6.9 7.0 7.0 7.1 6.7 6.8 6.8 6.9 7.0 7.0 6.7 6.7 6.8 6.8 6.9 6.9 6.6 6.7 6.7 6.8 6.8 6.9 6.6 6.6 6.7 6.7 6.8 6.8 6.5 6.5 6.6 6.7 6.7 6.8 6.4 6.5 6.5 6.6 6.6 6.7 6.4 6.4 6.5 6.5 6.6 6.6 6.3 6.4 6.4 6.5 6.5 6.6 6.3 6.3 6.4 6.4 6.5 6.5 45 665 12.8 12.6 12.4 12.3 12.1 11.9 11.8 11.6 11.5 11.3 11.2 11.0 10.9 10.7 10.6 10.5 10.3 10.2 10.1 10.0 9.9 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 6.9 6.9 6.8 6.8 6.7 6.6 6.6 670 12.9 12.7 12.5 12.4 12.2 12.0 11.9 11.7 11.5 11.4 11.2 11.1 11.0 10.8 10.7 10.6 10.4 10.3 10.2 10.1 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 6.9 6.9 6.8 6.7 6.7 6.6 675 13.0 12.8 12.6 12.4 12.3 12.1 11.9 11.8 11.6 11.5 11.3 11.2 11.0 10.9 10.8 10.6 10.5 10.4 10.3 10.1 10.0 9.9 9.8 9.7 9.6 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.7 8.6 8.5 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.4 7.4 7.3 7.2 7.2 7.1 7.0 7.0 6.9 6.9 6.8 6.7 6.7 680 13.1 12.9 12.7 12.5 12.4 12.2 12.0 11.9 11.7 11.6 11.4 11.3 11.1 11.0 10.8 10.7 10.6 10.5 10.3 10.2 10.1 10.0 9.9 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.5 8.4 8.3 8.2 8.1 8.0 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.4 7.4 7.3 7.2 7.2 7.1 7.0 7.0 6.9 6.8 6.8 6.7 685 13.2 13.0 12.8 12.6 12.5 12.3 12.1 12.0 11.8 11.7 11.5 11.4 11.2 11.1 10.9 10.8 10.7 10.5 10.4 10.3 10.2 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.6 7.6 7.5 7.4 7.4 7.3 7.2 7.2 7.1 7.0 7.0 6.9 6.8 6.8 690 13.3 13.1 12.9 12.7 12.5 12.4 12.2 12.1 11.9 11.7 11.6 11.4 11.3 11.1 11.0 10.9 10.7 10.6 10.5 10.4 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.4 9.3 9.2 9.1 9.0 8.9 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 7.0 6.9 6.8 695 13.4 13.2 13.0 12.8 12.6 12.5 12.3 12.1 12.0 11.8 11.7 11.5 11.4 11.2 11.1 11.0 10.8 10.7 10.6 10.4 10.3 10.2 10.1 10.0 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.6 8.5 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 6.9 6.9 15th Edition, 2013 HYDROLAB QUANTA °C 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0 5.5 6.0 6.5 7.0 7.5 8.0 8.5 9.0 9.5 10.0 10.5 11.0 11.5 12.0 12.5 13.0 13.5 14.0 14.5 15.0 15.5 16.0 16.5 17.0 17.5 18.0 18.5 19.0 19.5 20.0 20.5 21.0 21.5 22.0 22.5 23.0 23.5 24.0 24.5 25.0 25.5 26.0 26.5 27.0 27.5 28.0 28.5 29.0 29.5 30.0 700 13.5 13.3 13.1 12.9 12.7 12.6 12.4 12.2 12.1 11.9 11.8 11.6 11.5 11.3 11.2 11.0 10.9 10.8 10.6 10.5 10.4 10.3 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.4 8.3 8.2 8.1 8.0 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 7.1 7.0 6.9 705 13.6 13.4 13.2 13.0 12.8 12.6 12.5 12.3 12.2 12.0 11.8 11.7 11.5 11.4 11.3 11.1 11.0 10.8 10.7 10.6 10.5 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.5 9.4 9.3 9.2 9.1 9.0 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.6 7.6 7.5 7.4 7.4 7.3 7.2 7.2 7.1 7.0 7.0 710 13.7 13.5 13.3 13.1 12.9 12.7 12.6 12.4 12.2 12.1 11.9 11.8 11.6 11.5 11.3 11.2 11.1 10.9 10.8 10.7 10.5 10.4 10.3 10.2 10.1 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.7 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.6 7.5 7.4 7.4 7.3 7.2 7.2 7.1 7.0 715 13.8 13.6 13.4 13.2 13.0 12.8 12.7 12.5 12.3 12.2 12.0 11.9 11.7 11.6 11.4 11.3 11.1 11.0 10.9 10.7 10.6 10.5 10.4 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.5 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.8 7.8 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.2 7.1 720 13.8 13.7 13.5 13.3 13.1 12.9 12.7 12.6 12.4 12.3 12.1 11.9 11.8 11.6 11.5 11.4 11.2 11.1 10.9 10.8 10.7 10.6 10.4 10.3 10.2 10.1 10.0 9.9 9.8 9.6 9.5 9.4 9.3 9.2 9.1 9.1 9.0 8.9 8.8 8.7 8.6 8.5 8.4 8.4 8.3 8.2 8.1 8.0 8.0 7.9 7.8 7.7 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 7.1 725 13.9 13.7 13.6 13.4 13.2 13.0 12.8 12.7 12.5 12.3 12.2 12.0 11.9 11.7 11.6 11.4 11.3 11.2 11.0 10.9 10.8 10.6 10.5 10.4 10.3 10.2 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.8 8.7 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.7 7.6 7.5 7.5 7.4 7.3 7.3 7.2 730 14.0 13.8 13.7 13.5 13.3 13.1 12.9 12.8 12.6 12.4 12.3 12.1 12.0 11.8 11.7 11.5 11.4 11.2 11.1 11.0 10.8 10.7 10.6 10.5 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 7.9 7.9 7.8 7.7 7.6 7.6 7.5 7.4 7.4 7.3 7.2 Barometric Pressure (mm Hg) 735 740 745 750 755 760 14.1 14.2 14.3 14.4 14.5 14.6 13.9 14.0 14.1 14.2 14.3 14.4 13.7 13.8 13.9 14.0 14.1 14.2 13.6 13.6 13.7 13.8 13.9 14.0 13.4 13.5 13.6 13.6 13.7 13.8 13.2 13.3 13.4 13.5 13.6 13.6 13.0 13.1 13.2 13.3 13.4 13.5 12.8 12.9 13.0 13.1 13.2 13.3 12.7 12.8 12.8 12.9 13.0 13.1 12.5 12.6 12.7 12.8 12.9 12.9 12.3 12.4 12.5 12.6 12.7 12.8 12.2 12.3 12.4 12.4 12.5 12.6 12.0 12.1 12.2 12.3 12.4 12.4 11.9 12.0 12.0 12.1 12.2 12.3 11.7 11.8 11.9 12.0 12.1 12.1 11.6 11.7 11.8 11.8 11.9 12.0 11.4 11.5 11.6 11.7 11.8 11.8 11.3 11.4 11.5 11.5 11.6 11.7 11.2 11.3 11.3 11.4 11.5 11.6 11.0 11.1 11.2 11.3 11.3 11.4 10.9 11.0 11.1 11.1 11.2 11.3 10.8 10.9 10.9 11.0 11.1 11.2 10.7 10.7 10.8 10.9 11.0 11.0 10.5 10.6 10.7 10.8 10.8 10.9 10.4 10.5 10.6 10.6 10.7 10.8 10.3 10.4 10.4 10.5 10.6 10.7 10.2 10.3 10.3 10.4 10.5 10.5 10.1 10.1 10.2 10.3 10.4 10.4 10.0 10.0 10.1 10.2 10.2 10.3 9.9 9.9 10.0 10.1 10.1 10.2 9.7 9.8 9.9 9.9 10.0 10.1 9.6 9.7 9.8 9.8 9.9 10.0 9.5 9.6 9.7 9.7 9.8 9.9 9.4 9.5 9.6 9.6 9.7 9.8 9.3 9.4 9.5 9.5 9.6 9.7 9.2 9.3 9.4 9.4 9.5 9.6 9.1 9.2 9.3 9.3 9.4 9.5 9.1 9.1 9.2 9.2 9.3 9.4 9.0 9.0 9.1 9.2 9.2 9.3 8.9 8.9 9.0 9.1 9.1 9.2 8.8 8.8 8.9 9.0 9.0 9.1 8.7 8.8 8.8 8.9 8.9 9.0 8.6 8.7 8.7 8.8 8.9 8.9 8.5 8.6 8.6 8.7 8.8 8.8 8.4 8.5 8.6 8.6 8.7 8.7 8.4 8.4 8.5 8.5 8.6 8.7 8.3 8.3 8.4 8.5 8.5 8.6 8.2 8.3 8.3 8.4 8.4 8.5 8.1 8.2 8.2 8.3 8.4 8.4 8.1 8.1 8.2 8.2 8.3 8.3 8.0 8.0 8.1 8.2 8.2 8.3 7.9 8.0 8.0 8.1 8.1 8.2 7.8 7.9 7.9 8.0 8.1 8.1 7.8 7.8 7.9 7.9 8.0 8.0 7.7 7.8 7.8 7.9 7.9 8.0 7.6 7.7 7.7 7.8 7.8 7.9 7.6 7.6 7.7 7.7 7.8 7.8 7.5 7.5 7.6 7.7 7.7 7.8 7.4 7.5 7.5 7.6 7.6 7.7 7.4 7.4 7.5 7.5 7.6 7.6 7.3 7.4 7.4 7.5 7.5 7.6 765 14.7 14.5 14.3 14.1 13.9 13.7 13.6 13.4 13.2 13.0 12.9 12.7 12.5 12.4 12.2 12.1 11.9 11.8 11.6 11.5 11.4 11.2 11.1 11.0 10.8 10.7 10.6 10.5 10.4 10.3 10.2 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.6 8.5 8.4 8.3 8.2 8.2 8.1 8.0 8.0 7.9 7.8 7.7 7.7 7.6 770 14.8 14.6 14.4 14.2 14.0 13.8 13.6 13.5 13.3 13.1 12.9 12.8 12.6 12.5 12.3 12.1 12.0 11.9 11.7 11.6 11.4 11.3 11.2 11.0 10.9 10.8 10.7 10.6 10.4 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.9 8.8 8.7 8.6 8.5 8.5 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.9 7.8 7.7 7.7 775 14.9 14.7 14.5 14.3 14.1 13.9 13.7 13.5 13.4 13.2 13.0 12.9 12.7 12.5 12.4 12.2 12.1 11.9 11.8 11.7 11.5 11.4 11.2 11.1 11.0 10.9 10.7 10.6 10.5 10.4 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.8 8.7 8.6 8.5 8.4 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.8 7.8 7.7 780 15.0 14.8 14.6 14.4 14.2 14.0 13.8 13.6 13.5 13.3 13.1 12.9 12.8 12.6 12.5 12.3 12.2 12.0 11.9 11.7 11.6 11.5 11.3 11.2 11.1 10.9 10.8 10.7 10.6 10.5 10.4 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.2 9.1 9.0 8.9 8.8 8.7 8.6 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.0 8.0 7.9 7.8 7.8 785 15.1 14.9 14.7 14.5 14.3 14.1 13.9 13.7 13.5 13.4 13.2 13.0 12.9 12.7 12.5 12.4 12.2 12.1 11.9 11.8 11.7 11.5 11.4 11.3 11.1 11.0 10.9 10.8 10.6 10.5 10.4 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 9.0 8.9 8.8 8.7 8.6 8.5 8.5 8.4 8.3 8.2 8.2 8.1 8.0 8.0 7.9 7.8 790 15.2 15.0 14.8 14.6 14.4 14.2 14.0 13.8 13.6 13.5 13.3 13.1 12.9 12.8 12.6 12.5 12.3 12.2 12.0 11.9 11.7 11.6 11.5 11.3 11.2 11.1 11.0 10.8 10.7 10.6 10.5 10.4 10.3 10.2 10.1 9.9 9.8 9.7 9.7 9.6 9.5 9.4 9.3 9.2 9.1 9.0 8.9 8.8 8.8 8.7 8.6 8.5 8.4 8.4 8.3 8.2 8.1 8.1 8.0 7.9 7.9 795 15.3 15.1 14.9 14.7 14.5 14.3 14.1 13.9 13.7 13.5 13.4 13.2 13.0 12.9 12.7 12.5 12.4 12.2 12.1 12.0 11.8 11.7 11.5 11.4 11.3 11.2 11.0 10.9 10.8 10.7 10.6 10.4 10.3 10.2 10.1 10.0 9.9 9.8 9.7 9.6 9.5 9.4 9.3 9.2 9.2 9.1 9.0 8.9 8.8 8.7 8.7 8.6 8.5 8.4 8.3 8.3 8.2 8.1 8.1 8.0 7.9 Results from DOTABLES program at http://water.usgs.gov/software/DOTABLES/ Table generated Thursday 16-Feb-2012 11:34 EST Field Procedures 46 15th Edition, 2013 FLOW The main procedure described here primarily follows the discharge measurement procedure described in the 1994 TFW Ambient Monitoring Program (Schuett-Hames et al., 1994). Some modifications were suggested by the Washington State Department of Ecology or based on Ecology’s protocol (Kardouni 2011). The later 1999 TFW protocol calls for more cells and longer velocity averages, but Streamkeepers’ technical advisors consider the 1994 TFW protocols to have adequate accuracy for our program purposes. NOTE: Zero flows are important data; if you can’t measure flow, indicate one of the following: • No water visible. • Water in pockets only. • Water in channel, but no apparent flow. • Water flowing in channel, but level and/or velocity are too low to measure—in this case, record the wetted width and deepest depth that the flow rod can get to. EQUIPMENT NEEDED • • • • • • • • but in other cases they are separate monuments. (Check your reach maps, team leader, or program staff for more information.) If your site has such monuments, use them. If it does not, you should pick the best spot on that day: • The ideal site would be at least 5’ across, at least 3” deep, and have water that is flowing straight and not turbulently at ≥ 1 ft/sec. • If you can’t find an ideal site (as is likely to happen with smaller streams in the summer), find or create a site where the water is at least 3” deep and moving at ≥ 0.5 ft/sec. (I.e., compromise on width if you have to.) You can “create” such a site by making temporary “peninsulas” on the sides of the creek to concentrate the flow, using rocks/gravel/sand, or the sandbags in your field kit. • Look for variations in the amount of water you see flowing along the length of your reach, and measure at a spot where the flow is maximized and not running underground. • A suitable site should not have sidechannels, undercut banks, or flow obstructions such as boulders, logs, or aquatic vegetation. If a few large rocks are in the way, you can move them about six feet downstream. • You may walk outside your reach IF no water leaves or enters the stream in between. Velocity meter and staff (main instructions are for Swoffer 2100; special instructions for MarshMcBirney 2000 are at the end of this section) flexible measuring tape in 0.1’ increments 2 stakes pocket calculator timepiece sand-bags and ties, small shovel extra batteries (Swoffer: 9V; M-M: 2 D’s) data sheet, clipboard, pencil In this procedure, you will measure depth and velocity at 15-20 points across your stream. Back at the office, we will use your measurements to calculate the amount of water that the stream is discharging, recorded in cubic feet per second (“cfs”). For informational purposes, to better understand how discharge is calculated, see the illustration on the last page of this protocol. This procedure is best performed by two people: one taking measurements and the other recording. When to measure: Generally, you’ll measure flow each time you monitor each reach. If possible, wait until a day or two after major storms, to give the stream time to return to its baseflow. Also keep safety in mind—think twice about going into water above your knees. Where to measure: Streamkeepers has established permanent flow monitoring markers at some of its monitoring reaches. In many cases they are the cross-section monuments, Field Procedures 47 15th Edition, 2013 FLOW 2. Take the “PRIMARY” rotor/propeller bag from the “treasure box” in your kit. Record the rotor number, calibration number, and calibration date on your data sheet. SWOFFER 2100 STAFF: (2) For 6/10 depth setting, bring this 0.5 ft. mark… down to top of slide fitting… (1) Read depth here (in this case, 0.50 ft.) . PREPARING THE METER AND STAFF 1. While still on dry land, remove the velocity meter staff from its plastic-pipe case (see picture). Move the moveable rod up slightly. (Loosen or tighten the black knob on the slide fitting at the top, so that the sliding rod moves snugly.) At the bottom of the moveable rod is a boom that swivels. Swivel the boom to the 90° position. Take the orange protective cap from the boom and put it in your pocket. Field Procedures 48 3. Take the rotor/prop unit out of the bag. Make sure the number etched into the side of the unit is the same as that on the bag. If not, check the other bag, or write down the numbers on both the bag and the unit. Make sure the knurled nut on the end is snug. Then perform a hand-spin test: Hold the unit vertically by the steel rotor shaft with the prop facing up, and give a super-fast spin to the nut on top of the prop by “snapping” your fingers. If you hear a buzz, the rotor needs to be replaced—switch to the “SPARE” and return to Step 2. IF ANY ROTOR FAILS THE HAND-SPIN TEST, NOTE IT ON THE DATA SHEET AND INFORM THE PROGRAM MANAGERS UPON RETURNING THE EQUIPMENT. On your data sheet, mark the results of the test for the rotor you used. 4. Insert the rotor/prop assembly into the sensor boom on the staff. Use the 1/16” Allen wrench from the same bag as the rotor/prop to tighten the tiny set screw at the tip of the boom, just enough so that the rotor/prop assembly cannot be pulled off of the boom, plus a tiny bit extra. The prop should spin freely. Put the Allen wrench in your pocket. 5. Connect the cables on the meter and staff. The connector is “keyed” and only mates one way, so be very careful that you are aligning the connector ends properly. Push the connector ends together, and then twist clockwise until the connector clicks into the lock position. 6. Switch to the “CALIBRATE” position. The display should read the same calibration number as that given for the primary rotor/prop assembly. If the number is not the same but is within 10%, proceed—the computer will compensate for the difference. If the difference is >10%, try a fresh battery (see “Meter Troubleshooting” at the end of this section), and if that doesn’t work, start over with the spare rotor/prop. Record the meter calibration number on your data sheet. 7. Perform a count test: Rotate the switch to the “COUNT” position. Turn the prop slowly and confirm that the count increases by one for every quarter-turn of the prop. If not, try a fresh battery. On your data sheet, mark the results of the count test. 15th Edition, 2013 FLOW 8. Perform a blow-spin test: Hold the rotor/prop assembly with the prop facing up, and blow a strong, steady, sustained breath of air to give the 3” prop a chance to overcome inertia. (If you are using an older 2” prop, use a short hard puff.) Right after you stop blowing, hit the “RESET” button on the meter and allow the rotor to coast to a stop. If the count is less than 300 consistently or if the prop stops abruptly instead of coasting slowly to a halt, try to: • Back off slightly on the set-screw, or • Take apart the rotor, rinse it in clean water and try again, or • Switch to the “SPARE” and return to Step 2. On your data sheet, record the results of the blow-spin test for the rotor you use. IF ANY ROTOR FAILS THE BLOW-SPIN TEST, INFORM THE PROGRAM MANAGERS UPON RETURNING THE EQUIPMENT. 9. When satisfied that the flow meter is operating correctly, turn the switch “OFF”. MEASURING FLOW 1. Record on your data sheet: a) the time, and b) the bank you’ll be starting at (NOTE: left and right are always facing downstream). 2. Determine the nominal interval for your measurements: a) At the point where you have decided to measure flow, stretch a tape across and above the wetted portion of the stream channel perpendicular to the direction of flow. (This may not be exactly perpendicular to the stream banks.) Use spring clamps to secure the tape around vegetation, large rocks, or stakes. b) On your data sheet, note the tape readings for the wetted edges to the nearest 0.1’. Calculate and record the wetted width of the stream by subtracting one wetted edge from the other. Divide the wetted width by 10 to find the MAXIMIUM INTERVAL and record it on the data sheet. Do not exceed the MAXIMIUM INTERVAL between measurements even outside of the “propturning” portion (see below). c) Determine the area along this line where the prop turns—i.e., don’t include portions where the stream is too shallow or the water isn’t moving. (This must be at least 0.1 inch inside of the wetted edges you have Field Procedures 49 recorded.) On your data sheet, note the distances on the tape corresponding to the edges of the “prop-turning” portion. Calculate and record the “prop-turning” width on the data sheet by subtracting one from the other. d) On your data sheet, divide this “prop-turning distance” by 20, then round UP any decimals to the nearest tenth of a foot. This will give you an average interval that will yield 15-20 measuring-point cells across the “propturning” area. (For example, if the area is 12.2’ wide, 12.2’/20 = 0.61’. If you round UP to 0.7’, you will have about 12.2/0.7 or 17 cells.) NOTE: The MINIMIUM INTERVAL distance is 0.3’, regardless of what you rounded up to. So in a creek smaller than 4.5’ across, you’ll have fewer than 15 cells. 3. Zero readings at wetted edges: At both wetted edges (see above), you’ll need to record the tape reading in the first and last blank in the flow data table; the depth and velocity (both zero) have already been recorded on the data sheet for you. If the bank is undercut (try to avoid this!), you’ll have to estimate how far back the water goes. (You can do this by putting a stick into the undercut and then measuring this distance on the stick.) 4. Proper stance: Put the velocity meter’s strap around your neck and enter the stream downstream of the tape. When taking measurements, stand with the wading rod at arm’s length and your feet upstream and downstream of each other, off to the side of where the water flows past the rod. You will be facing upstream at about a 45° angle. Hold the rod so the propeller faces into the flow. 5. Intervals for measurements: Your nominal interval will be the one you calculated on your data sheet. However, your actual intervals should be: • larger in non-prop-turning areas or places where water depth or velocity are relatively small or uniform smaller in places where water depth or velocity are relatively large or are changing rapidly Intervals should be: • no greater than 1/10 the wetted width of the stream (MAXIMIUM INTERVAL) • 15th Edition, 2013 FLOW of the prop (see sketch). • no smaller than 0.3’ (MINIMIUM INTERVAL) You need to take readings even in non-propturning areas, where you’ll just record distance, depth, and in the velocity field either: “insf/d” for insufficient depth, “insf/v” for insufficient If it does not, then rotate the rod to one side or the other, until the prop faces directly into the current with the tell-tail straight out behind it (see sketch below). Take your measurement with the prop turned into the current at this angle. velocity or “insf/dv” for both (see “LowVelocity Conditions” below). BE SURE TO TAKE READINGS 0.3’ TO EITHER SIDE OF “PROP-TURNING” EDGES, unless those edges are right next to the wetted edges. 6. Taking readings—general procedure for water between 0.3 and 2 feet deep: a. Set the rod on the stream bottom and record the tape reading on your data sheet, to the nearest tenth of a foot. b. Adjust the moveable rod as needed to set the tip of the prop at water level. The staff should be vertical, which you can determine by briefly letting go of it. Read the stream depth from the large scale on the moveable rod, at the point where it enters the top of the slide fitting. (See picture earlier in this section.) Note that the scale reads downward, intervals are in tenths of a foot, and foot-marks are triple lines. Record the water depth from the staff, to the nearest hundredth of a foot. (You will have to estimate between the 0.1’ markings on the staff.) Estimate, to the nearest 10°, the angle you rotated the rod, and record it on the data sheet. (It doesn’t matter whether you rotated the rod left or right—just record the number of degrees you had to rotate it.) If you did not need to rotate it at all, write 0. (If the stream flow were completely reversed at your point of measurement, i.e. flowing back upstream, and you had to turn the rod completely around, you would record an angle of 180°.) c. Place the prop at 6/10 the distance from the water surface to the stream bottom. You can do this easily by lowering the moveable rod until the top of the slide fitting matches the marking for your stream depth on the smaller rod. For example, if your depth is 0.4 feet, slide the rod down to the fourth notch on the smaller rod. (Exception: do not go so far that the prop hits the stream bottom.) NOTE: If the water is turbid and you can’t see the tell-tail, you should be able to feel the “sweet spot” where the current isn’t trying to push the rod to either the left or right. Then compare the angle you see on the double-rod to the angle of the overall current. d. The tell-tail (piece of colored twine attached to the back of the prop/rotor fitting) will ordinarily point downstream in line with the axis Field Procedures e. Turn the meter switch to “DISPLAY AVERAGING” (between the Min and Max settings). Press and release the RESET button to zero the display. After approximately 25 seconds, the meter will display a velocity. Record this reading in the “velocity” column on your data sheet. f. 50 Proceed across the stream, taking your readings, ending at the far wetted edge. 15th Edition, 2013 FLOW g. If any velocity reading is different by a factor of 2 than the previous one, the recorder should ask the sampler to confirm that reading. h. COMMON SENSE & FLOW READINGS: Use your common sense to consider whether the velocity on the meter jibes with how fast the water seems to be moving. Certain conditions can cause the meter to mis-read. If you doubt a reading, take another, then a third to confirm. If possible, record all of these data points along with an explanation of which ones you think should be ignored, and why. If problems persist, see the “Troubleshooting” section later in this protocol. i. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data, which will generally be the person with the most experience or knowledge. j. Recheck the meter calibration number (switch to “CALIBRATE”). If the number has changed, record the new number alongside the first number on your data sheet. k. Turn the meter off when finished taking readings, and see storage and transport instructions at the end of this section. 7. Procedure for water >2 feet deep: First, seriously consider whether it’s safe for you to be in the stream! If you’re sure it is (you’ll need chest waders), you will need to take two velocity and angle measurements, at 2/10 & 8/10 of total depth. To do this: a. Put slashes across the velocity and angle boxes, to make room for the two readings you will take. b. For the 2/10-of-depth reading, take the depth you measured and multiply it by 0.2, then lower the rotor assembly by this amount on the larger rod. An easy way to calculate this in your head is to double the depth number and move the decimal one place to the left. For example, if your depth shows 2.8, doubled is 5.6, and moving the decimal left makes it 0.56. You would drop the rotor assembly by this amount on the larger rod scale to 2.24 (i.e., 2.8 minus .56). Record velocity and angle at this point, as described above. c. For the 8/10-of-depth reading, drop the rotor to 0.2 of the water’s depth, the same Field Procedures number you calculated above. Move the slide fitting to that point on the large rod. In the example above, the rotor would drop to 0.56 feet. Record velocity and angle at this point, as described above. 8. Procedures for low-velocity conditions: a. If at a given measuring point, the water isn’t moving fast enough to turn the prop, write “insf/v” (“insufficient velocity”) on the data sheet. b. If the prop turns, but erratically, measure the velocity a second time. If the difference is <20%, keep the first reading. If the difference is >20%, take a third reading, and record the average of all three. 9. Procedure for water <0.3 feet deep: For very shallow water, don’t worry about the depth at which you set the prop—put it at any depth where the prop will turn. Record distance, water depth, and velocity as usual. (Note if the prop is partway out of the water.) However, if the shallowness is clearly impacting your velocity measurements, try one of the alternative low flow methods on the next page suggested by the U.S. Bureau of Reclamation (Perry, 2003). 10. Gunk on the prop: If there is a lot of organic matter in the stream (particularly filamentous algae and particulates), you may find the prop becoming impeded and turning erratically or not at all. The rotor/prop unit may have become dirty inside. Take off the rotor/prop unit using the 1/16” Allen wrench and try rinsing it in clean water or squirting clean water up the rotor shaft. If that doesn’t help, unscrew the knurled knob, remove the rotor shaft, and gently clean both it and the bore hole in clean water. You may have to do this several times in certain conditions. 51 15th Edition, 2013 FLOW ALTERNATE LOW-FLOW PROCEDURES determination can be made in the office as whether to apply a correction factor.) BUCKET METHOD: If you can capture the flow (from a culvert or waterfall) in a bucket or other container, simply time how many seconds it takes to fill it. Record 3 reps, and then record the average. Measure the volume of the container and convert to cu. ft. (128 oz. = 1 gal. = 0.134 cu. ft.). Record the results with every step labeled clearly so office staff can verify the results. STREAM GAGES: Your stream may have a water-level gage installed on it, or we may be able to install one if you’re willing to do the legwork. Over the course of time, dual readings from both the flow meter and gage yield a formula that enables us to estimate discharge simply by reading the gage. (We also have to calibrate the gage by periodically making dual readings and measuring the channel cross section.) ONE-POINT “HYDRAULIC” METHOD: Find or create a small ditch that confines the water, using rocks or sandbags as needed, creating a section as rectangular in cross-section as possible, a few feet long if possible, and deep enough to submerge the prop of the meter. (Also ensure you’re measuring at a spot where significant amounts of water aren’t flowing under the gravel; you may have to walk several hundred yards to determine this.) Then: If you have a gage at your site, simply record the water height and units on your flow field sheet. Read the gage both before and after measuring flow, if possible. Please see Streamkeepers staff if you think a gage is or can be installed near your reach. FLOATING-OBJECT METHOD: This method will produce an estimate of flow when other methods aren’t available (Murdoch et al. 1996): 1. Find one good spot for a velocity reading: a) halfway between the upstream and downstream ends of your ditch; b) at a place where the tell-tail points straight back; and c) at halfway depth. If the prop does not turn freely at this point, try to find a spot at which it does. 2. Take a velocity measurement at that point: set the meter to "Velocity/Max,” take 3 readings, record and average them. (If you still can’t get the prop to work, estimate the velocity by marking off the length of your ditch and floating a small twig down its length ten times. Divide the number of feet by the average number of seconds to get the velocity [all to the nearest tenth].) 3. Measure and record the channel depth and width at the spot you measured. 4. Multiply Velocity x Depth x Width and round to the nearest tenth or else to the first digit with an actual number (e.g., .04 or .003). This is your flow measure. (Note: this method is a way to estimate flow under poor conditions and does not account for friction so it may result in an overstated flow value. Provide all relevant information so a Field Procedures 1. Find a place with the most even flow and flat bottom. 2. Mark off a 10-ft course. 3. Throwing twigs in above the starting line, then time them from start to finish. 4. Throw them in at multiple places across the creek to get an average time. 5. Divide ten by the average time to get the average velocity in ft/sec. 6. Estimate average depth & width to get a cross-sectional area. 7. Multiply the above by a 0.9 friction coefficient for a smooth-bottomed stream or 0.8 for bottoms with rocks or plants. 8. Round to two significant figures (probably one decimal place). 52 15th Edition, 2013 FLOW MONITORING FLOW BETWEEN SESSIONS b) Examine the cords and connectors for wetness, bad connections, or any other obvious problems, taking corrective action where possible. c) Try taking the battery out from the back panel, checking for wetness or corrosion, and putting it back in if it looks okay. Sometimes this simple step can reset the circuits. If this doesn’t work, try replacing the battery. d) Try the blow test again. If it fails, you can either take apart the rotor and rinse all the parts, or switch to the spare rotor. e) IF YOU CONTINUE TO EXPERIENCE DIFFICULTIES, NOTE THE NATURE OF THE PROBLEMS ON THE DATA SHEET AND DISCONTINUE FLOW MONITORING. INFORM PROGRAM STAFF UPON RETURNING THE EQUIPMENT. You might want to measure flow between quarterly monitoring sessions, to learn more about extreme high and low flows in a stream, or about how flow changes during a storm. Therefore, if… you want to perform additional flow sampling, • a field kit is available, • it is SAFE to monitor, and • you have a team of at least two, …you are welcome to borrow a field kit and data sheet at any time. • METER TROUBLESHOOTING 1. If the meter falls in the water, open the battery compartment on the back as soon as possible by twisting the set screws loose by hand. Dry the battery terminals and cable connections, and let the compartment air dry as much as possible before replacing the cover. Hand-tighten the set screws. 2. If the prop isn’t spinning freely: a) You may be at a spot in the stream with no current (or almost none). A sign of this would be that the tell-tail is drooping. If the tell-tail is pointing to the side, you may need to rotate the staff to face into the current. b) If the tell-tail indicates current and the prop isn’t spinning, try the “Gunk on the prop” cleaning procedure described earlier. c) Try the hand-spin and blow-spin tests again. If a test fails, switch to the spare prop and start the flow measurement procedure over again from the beginning. Note problems and how you dealt with them on your data sheet. 3. If the velocity readings appear inconsistent or illogical as you’re proceeding across the stream, try the following fixes and test them by turning the meter to “Count” and letting the prop turn in the stream; the numbers shouldn’t skip or stop (unless the current is very slow). a) Try turning the meter on and off again. Sometimes this will reset the circuits. Field Procedures TIPS FOR DATA RECORDING 1. Write legibly and be sure to record the data in the units and number of decimal places called for on the data sheet. 2. The data recorder should repeat measurements back out loud to the flow sampler to avoid mistakes. 3. The data recorder should be alert for inconsistencies in the progression of the numbers and bring any suspect sudden changes to the attention of the flow sampler for verification and resampling if necessary. 4. Use common sense when recording readings. If the water appears to be moving faster or slower than the meter is reading, consider going over the METER TROUBLESHOOTING steps in the prior section. 5. Zero Flow – describe conditions carefully. Refer to grab sample protocol 53 15th Edition, 2013 FLOW METER STORAGE AND TRANSPORT 1. When swiveling the boom mechanism, always hold it by its base and not by the rotor assembly. 2. NEVER transport the staff with the rotor/prop attached. Take off the rotor assembly, and replace the orange protective cap between sites. Return rotor/prop unit and Allen wrench to the treasure box. If you are going to another monitoring reach that day, you can keep the rotor/prop and Allen wrench in your pocket. 3. DO NOT wrap the cord around the wand before storing in the plastic tube to avoid causing shorts in the electrical cables. The preferred method of storage is to place the wand in the tube “head” first and drop the cord down inside when the wand is about halfway in, then insert the rest of the wand with the “foot” part at the top and the tell-tail tucked under so it does not get frayed. 4. At the end of each monitoring day, always be sure to remove the rotor/prop assembly and store staff, meter, rotor/prop assembly, protective cap and Allen wrench in their proper places. If possible, dry these parts with the rags in your field kit before storing. MEASURING RIVER/STREAM STAGE At sites with stage-gages (rulers mounted in the stream to a post or pier), record the stage, both before and after measuring flow, below the flowcell data on the data sheet. In some cases, stage is measured by simply measuring the water level at some monumented point, or by measuring topdown from a set point (such as the top inside diameter of a culvert), in which case the value would be a negative number. Check the site description to see how to measure stage there. Indicate the method used on the data sheet. Field Procedures 54 15th Edition, 2013 FLOW Measuring Velocity Marsh-McBirney® Model 2000 (adapted from WA Dept. of Ecology—Kardouni 2011) NOTE: Ecology’s Stream Hydrology Unit (SHU) does not use Marsh-McBirney meters nor recommend their use. Ferrous metals can corrupt the electromagnetic field within which the meter measures velocity, and it is extremely difficult if not impossible to determine when, where, and to what extent the field is altered. (Casey Clishe, SHU, personal communication May 2013). Given this situation, it might be particularly problematic using the M-M meter to measure the flow in or near a steel culvert. The Marsh-McBirney® 2000 consists of a transducer probe, cable, and signal processor. The probe emits an electromagnetic frequency used to measure velocity. The Marsh-McBirney® wading rod has an adapter capable of holding the transducer probe. • Attach transducer probe to wading rod. • Turn meter on. • If units indicated are not FT/S, toggle between to FT/S by pressing the On and Off keys simultaneously. • Meter is already set to Fixed Point averaging (FPA) of 30 seconds. • The wading rod should be set to the appropriate depth—see the “Taking Readings” section earlier in this protocol. • Place the probe in the stream with the round end of the sensor facing upstream. • The time bar provides an indication as to the amount of time left until the display is updated. Wait for the appropriate time delay and then record the stream velocity. Handling: The transducer probe’s instrumentation is fragile; protect the probe from bumping. Factory calibration: The meter should be sent to the factory for calibration at least once a year. The factory calibration report will indicate meter bias prior to calibration, which can be used to qualify data as needed. Questions? Refer to the manual, in the same bag with the meter. Zeroing the meter: To ensure accurate measurements, zero the meter at least once a week during use; however, it is preferable to zero it at the beginning and end of each day of use. First clean the sensor, because a thin film of oil on the electrodes can cause noisy readings. Then place the sensor in a five gallon plastic bucket of water, keeping it at least three inches away from the sides and bottom of the bucket. To make sure the water is not moving, wait 10 or 15 minutes after you have positioned the sensor before taking any zero readings. Use a filter value of 5 seconds. Zero stability is ± 0.05 ft/sec. • To initiate the zero start sequence, press the STO and RCL keys at the same time. You will see the number 3 on the display. • Decrement to zero with the 6 key. • The number 32 will be displayed. • The unit will decrement itself to zero and turn off. The unit is now zeroed. Field Procedures 55 15th Edition, 2013 FLOW How Flow is Calculated using TFW protocols Streamkeepers flow abbreviation definitions LBWE = Left Bank wetted edge of dry land. RBWE = Right Bank wetted edge of dry land. WW = Wetted width; the difference between wetted edges. Max∆ = MAXIMUM INTERVAL; 1/10th the wetted width. LBPT = Tape measurement at LB "prop-turning" edge. RBPT = Tape measurement at RB "prop-turning" edge. PTW = "Prop-turning" width; the difference between "prop-turning" edges. Nom∆ = NOMINAL INTERVAL; the "prop-turning" width divided by 20. Insf/d = Insufficient depth, water too shallow for prop to turn. Insf/v = Insufficient velocity, water too slow for prop to turn. Field Procedures 56 15th Edition, 2013 PHOTOS SUMMER PHOTOS EQUIPMENT NEEDED—BASIC • • • • (See sample photo log below) camera with SD card and charged battery photo log on data sheet or in camera case knowledge of position of “zero-point” (central monitoring point) or cross-section transect for your reach, from your handdrawn map, written description, or verbal instructions data sheet, clipboard, pencil 1. Make sure the date is right on the camera— if not, fix it (see “Camera Use”). 2. If you aren’t doing physical habitat measurements at this site, take photos upstream and downstream from your site’s “zero point” (central monitoring point), from mid-channel. 3. If you are doing physical habitat measurements at the site, do the following: EXTRA EQUIPMENT NEEDED FOR PHYSICAL HABITAT SUITE (Optional as of 2005): • • • • a) Leave the Cross Section tape, string, and bankfull flagging still attached. Cross Section tape and string still stretched across stream 2nd 100-foot tape, to stretch along baseline flagging tape, stakes Large Woody Debris and Erosion/Revetment protocols b) Stretch a tape along your baseline. Refer to your hand-drawn reach map or written description of zero-point location and compass bearing if necessary. c) Photograph: Photos provide a visual record of stream and riparian features which are archived in the Clallam County Water Resources database. Streamkeepers’ protocols call for different types of photos during the different quarterly monitoring sessions. Volunteers are also welcome to take additional photos at any time. i) The entire width of the cross-section transect, with three pieces of flagging tape hanging from the string, taken from downstream at mid-channel (this may require more than one photo). On the photo log, indicate how many feet the photographer is standing down-stream of the crosssection line. The camera is fully automatic, including exposure, focus, and fill-in flash. In rainy weather, keep the camera in your shirt pocket or close to your body to minimize fogging. For more camera instructions, see the “Camera Use” section. ii) Photos of where lbfull and rbfull were located, showing the entire bank with a flagged stake at the bankfull point. iii) Views upstream and downstream from the cross-section line, from midchannel. Fill out the Photo Log on the data sheet and include all relevant information as you take photos (see samples below). Abbreviations that you can use are printed below. iv) Photos of the string & tape where they attach to the lbm and rbm. Try to have a person or other familiar object in each photo as a size reference—but be sure not to block whatever the photo is supposed to show! Also, if possible, try to include a landmark—a culvert, bridge, fence, big rock, or other structure—that may help locate the photo’s location. Field Procedures 57 15th Edition, 2013 PHOTOS WINTER PHOTOS 1. Make sure the date is right on the camera— if not, fix it (see “Camera Use”). 4. Also take photos of the following features. For each feature, indicate on your photo log the distance from your zero-point, and the direction (u/s or d/s). 2. Take 4 photos from along the cross-section transect or zero-point of your site (see diagram on next page): a) Each piece of large woody debris (LWD), with a large enough field of view to see the surrounding channel and riparian area. (If you aren’t doing the Large Woody Debris protocol, take photos of any large wood that seems either to provide fish refuge or help shape the channel at some flow level.) a) Stand along the cross-section transect on one bank. Take a photo facing across the creek angling upstream, showing the opposite bank and riparian area. NOTE: Aim these shots so that the cross-section transect or centerline of the site is in the frame, but near the edge. (Either get the opposite-bank monument in view, or imagine where it would be.) b) Any eroded or revetted areas, if you have not already photographed them during a recent Streamwalk (see separate chapter). Here you may need to pause and perform the Erosion/Revetment protocol (or at least read the definitions therein). b) From the same position, take a similar photo facing across the creek angling downstream. c) Now cross the creek if possible (in winter time this may not always be possible to do safely!), stand along the cross-section transect on the opposite bank, and take a photo across to the other side and angling upstream. c) Any interesting or problem areas: i) wildlife signs: redds, tracks, scat, etc. ii) fish passage problems iii) anything causing habitat problems iv) new human-made structures 5. Also take shots of volunteers at work or play that we might be able to use as mementos or promotional materials. Be sure to record everyone’s initials. d) From the same position, take a photo facing across the creek and angling downstream. Take photos of anything else of interest, explaining the reason for the photo on your photo log. (See Summer Photos above for examples.) 6. Check “Yes” in the “Photos taken” box on your data sheet, and write the initials of the person who completed the photo log. If you didn’t take photos at this site, check “No” in this box. 3. Check “Yes” in the “Photos taken” box on your data sheet, and write the initials of the person who completed the photo log. If you didn’t take photos at this site, check “No” in this box. SPRING PHOTOS: None required, but see 3c & 4 under “Summer Photos.” FALL PHOTOS: These are described in the “Benthic Macroinvertebrate” protocol. Field Procedures 58 15th Edition, 2013 PHOTOS WINTER PHOTOS flow Photo #1: Field of view incorporates center-transect at right edge and shows as much of the opposite bank as possible (use wide angle) Cross-section transect or centerline of reach Photo #2: Similar to Photo #1, with center-transect at left edge of photo Photo vantage point from one bank, for Photos 1 & 2. (Photos 3 & 4 will be taken from the opposite bank, if it’s accessible.) Stream banks ABBREVIATIONS TO USE WITH PHOTO LOG (pasted on the inside back cover of the photo log) u/s, d/s = upstream, downstream LB, RB = left bank, right bank (when facing downstream) [#]’ = number of feet (along baseline from zeropoint, unless otherwise indicated) @ = at ch = channel X = cross, across X-Sec = cross section trans = transect pt = point STREAMKEEPERS OF CLALLAM COUNTY -- PHOTO LOG Site Name: Date: Morse 1.1 Photos taken at this site on this date? Yes X No 8 / 8 /08 Camera: 3 Samplers Initials: BDD FOR SUMMER & WINTER PHOTOS: AT SITES WITHOUT ESTABLISHED CROSSSECTION, USE CENTRAL SAMPLING POINT (A.K.A. "ZERO POINT") AS CENTRAL POINT FOR PHOTOS. Photo Log: fill in the log below completely for each picture including where it was taken from Frame # Subject Vantage Point 100-0023 x-sec tape 20’ d/s at mid-ch 100-0024 Facing u/s x-sec line, mid ch 100-0025 “ d/s “ 100-0026 LWD @ 35” u/s of zero-pt LB 100-0027 Logjam @ 80’ u/s of zero-pt. 30’ d/s of jam 100-0028 Erosion on RB 80-95’ u/s of zero-pt. LB 100-0029 Poison Hemlock @ 100’, LB 10’ away Field Procedures 59 15th Edition, 2013 PHOTOS ANYTIME PHOTOS 1. Photos taken outside of regular monitoring when no data sheet is used must be recorded on the Photo Log inside the camera case. See example in camera case Photo Log below. 2. Whenever you change the date, location, or sampler, you need to make a “breakout” line in the log that makes this change absolutely clear (see example below). STREAMKEEPERS OF CLALLAM COUNTY *** LOG FOR PHOTOS ONLY IF NOT PART OF A REGULAR MONITORING VISIT *** Camera #: 4 Location: Home Frame # 100-0030 ---Morse ---Morse 100-0031 --8/9/08 --8/9/08 100-0032 Date: 8/8/08 Initials: BDD Subject Carol Dunlap calibrating pH Creek ~30’ d/s of Discovery Trail Bridge-------------Bridge-------------Poison Hemlock on RB Ennis u/s of Ennis Creek Rd Unknown pipe input on LB THE SCOOP ON YOUR PHOTO LOGS & PHOTO DATA SHEETS A picture can be worth 1000 data points - that’s why we include photos in our monitoring program. When you return your camera, the photos are down-loaded and then “processed” by lightening or darkening parts as needed, attaching information from your photo logs to the photos, organizing and storing the photos in a systematic way, and copying these files into the Clallam County Water Resources database, right along with the rest of your data. But to get this all right, we need your help! Please note the following: • All entries in the photo log need to clearly indicate who, what, when, & where. • Correctly entering the camera # and frame # is essential for matching the photos to your photo log entries. Field Procedures 60 15th Edition, 2013 PHOTOS CAMERA USE Instructions for the Fuji XP10 Digital Camera The Fuji XP10 is flexible and easy to use. The camera has been set for automatic operation which should provide good pictures in all field conditions. Please do not change any of the settings other than those described below. Please insert your hand through the camera strap for safekeeping. Turning the Camera On and Off Press the small button on top and hold it down until an image appears on the screen, and the blue light comes on. Press the small button again to turn the camera off. Framing the Picture Position the main subject in the focus area and use the zoom buttons to frame the picture in the screen. Press W to zoom out or T to zoom in. Focusing and Shooting The camera will focus on whatever you see in the center of the screen. Press the shutter button (large button on top of the camera) halfway down to activate the auto-focus. When focus is obtained, two beeps will be heard. Press the button down the rest of the way to take the picture. Make sure you hold the button down until you hear the shutter click. In low light, the shutter will be slightly delayed while the scene is illuminated by the automatic flash. In the unlikely event focus is not obtained, a red message “AF!” will appear on the screen. In that case, find another object at the same distance from you, press the button half-way down to obtain a focus on that object, then, while keeping the button pressed halfway, move the camera to again view the picture you wish to take. Double Beep Press Halfway Click Press the rest of the way down Checking the Picture In order to check the picture, press the review arrow button on the back of the camera. If the picture is satisfactory, note all required information in the photo log sheet. If not, delete the picture and retake it. While in this mode, you can move back and forth between the stored pictures using the right and left sides of the Menu/OK button on the back of the camera. You can also zoom in on a picture you are viewing by using the zoom lever on the upper-right back of the camera. Press the shutter button to return to shooting mode. Field Procedures 61 15th Edition, 2013 PHOTOS Deleting Pictures To delete a picture being viewed, push the top of the Menu/OK button. A message will appear on the screen asking if you wish to erase the picture. To do so, again push the top of the Menu/OK button to select “OK” on the screen, then press the OK button. To exit without erasing, press the bottom of the Menu/OK button to select “Cancel” and press OK. Entering Data on Log Sheet When in the viewing mode, data for that picture is displayed on the screen. The frame number for that picture appears at the upper-right corner in the format XXX-XXXX. It is critical that this be entered on the log sheet, along with the descriptive information for the photo (see Photo protocol), the camera number, the site name, the date, and the initials of the photographer. If you get lost in the Menus, don’t start randomly hitting buttons! Get out by hitting the “DISP/BACK” button at the bottom of the back side. Charging the Battery In viewing mode, a battery icon appears at the lower right side of the screen, showing the battery state. If this is blinking or solid red, the battery needs to be recharged. The charger is in the “treasure box” of the “clean bag” of the Streamkeeper field kit. Turn camera off before removing the battery. With the camera in the position shown, locate a small slider button marked “OPEN” in the center of the bottom. Slide this away from you and then to the right, and the cover will release. Raise it as shown in the figure. The Lock Lever battery is held in place by an orange tab. Push this to the left and the battery will pop up. Insert the battery into the charger with the orange stripe on the left and the terminals facing down. The charging indicator will glow yellow when the battery is charging and green when it is fully charged. If it blinks yellow, remove the battery – there is a charging problem. Insert the battery with the orange stripe on the battery next to the orange tab on the camera. Push it in and it will snap into place. Lower the cover and push to the left to latch. Be sure that it is securely closed and snaps into place. Monopod Mount A monopod is supplied in your kit, which can be used to steady the camera in very low light situations. This can be screwed into a socket on the bottom of the camera. Field Procedures 62 15th Edition, 2013 PHOTOS SETTING MENUS FOR THE FUJI XP10 DIGITAL CAMERA Under normal circumstances, when the camera is turned on it will have already appropriate settings. However, should the settings be changed, the following instructions show how to go through the setting menus and select the proper options. DATE/TIME will appear just for a few seconds when you first turn on the camera. Confirm that these are correct. If not, see instructions below. INITIAL SCREEN: After the date disappears, the screen should show a view of whatever the lens is looking at, with various types of information on the screen and no grid. If there is no information on the screen, or there’s a grid, double-click the DISP/BACK button until the grid is gone and the information shows. (There are three possible views: information with grid, information only, and no information.) About the DISP/BACK button: This button, located at the bottom underneath MENU/OK button and the playback arrow, is easily pushed by mistake. AVOID “SILENT” MODE: If the display shows the SILENT mode symbol at top center: get out of it by pressing and holding the DISP/BACK button until that symbol goes away. , STREAMKEEPERS’ PREFERRED MENU CHOICES: This procedure makes use of selection buttons on the back of the camera as illustrated on the right. (continued on next page) Field Procedures 63 15th Edition, 2013 PHOTOS Press MENU/OK to display the Shooting Menu. 1. The menu opens with “SHOOTING MODE” highlighted. Press the right selector button to show options. Press the up or down buttons until “SR AUTO” is highlighted. Press OK. 2. Press the down selector button to highlight ISO. Press the right selector button to display options. Press the up or down buttons to select AUTO. Press OK. 3. Continue in this way to access all the items in the shooting menu, changing the various items if needed to those in the following list: Shooting Menu: Shooting Mode ISO Image Size Image Quality Fine Pix Color White Balance Continuous Face Detection AF Mode Movie Quality SR Auto Auto 12M N STD N/A Off On N/A N/A While viewing the Shooting Menu, press in sequence the left, down and right selector buttons to bring up the Setup Menu. As above, press the right button to access the options, and set the menu items. Press OK when done. Setup Menu: Date/Time Time Difference Language Silent Mode Reset Format Image Display Frame No. Use right, left, up, down buttons to set date and time. Home English Off DO NOT CHANGE. This resets all settings to factory defaults. DO NOT CHANGE. This erases all data from the memory card. 3 SEC Cont. ----Now skip down to the following items, and ignore the others: LCD Mode Auto Power Off Digital IS Red Eye Removal Save Org Image On 2 MIN Off On Off WHEN FINISHED, PRESS THE DISP/BACK BUTTON (below the small arrow) TO LEAVE THE MENUS. Field Procedures 64 15th Edition, 2013 FISH AND WILDLIFE SIGNS EQUIPMENT NEEDED WILDLIFE The visual observation approach the five senses field guides if you have them & are inclined to recommended below can yield valuable information on the presence and use them absence of wildlife and their relative • data sheet, clipboard, pencil abundances in different survey areas. For identification, there are many publications and Anytime you visit your reach, you will note any keys available to help you. The animal-tracks signs of fish or wildlife. You’ll be most likely to key in your field kit will help since most wildlife observe animal signs when you first arrive at do not appreciate human observers and hide your site, but be open to observations that may from view. Or you may wish to bring a occur at any time. How detailed and technical knowledgeable partner (such as an Audubon you wish to get is up to you, but even such member) to help you. information as “about six little brown birds,” “a BIRDS few fish fry about 2” long,” or “tracks-raccoon?” can be useful to biologists. The UW Birds may be the easiest creatures to spot. Nature Mapping project will accept observations Look and listen for them as you walk into your identified to species level only, so if you do reach. Take into consideration that different know the specific or Latin name for the creature species inhabit different layers of the you observe, be sure to list it. vegetation, from the dense, shrubby • • undergrowth to the top of the canopy. Note: Only write what you know—if you’re taking a guess, indicate that it’s a guess and why you’ve guessed it. Note the locations where you see and hear birds both spatially and vertically. Record the species that you are able to identify by sight or sound. Also document any evidence you see that birds are present, such as nests, egg shells, feathers, or tracks. FISH Your best bet is to quietly walk up to a pool, preferably not casting a shadow on it. If you’re lucky, you may see some fish-like shapes holding still or darting around. Other possible sightings include spawners in riffles or pool tailouts, carcasses, or redds (salmon and trout nests), which are elongated oval mounds in the streambed that are algae-free, often with a depression on the upstream side. HERPS Herps (reptiles and amphibians) are more secretive than birds. The best places to look for them are under rocks and logs in damp spots, especially along the stream's wetted edges. Take care not to create too much disturbance on the fragile stream banks, and make sure you return all logs and rocks to their original positions. There is a juvenile salmonid ID book in your field kit, but these are almost impossible to identify without catching them; “salmonid spp.” would cover any salmon or trout that you might find. If you investigate your watershed and consult your local fisheries biologist or Streamkeeper staff, you will be able to make a pretty good guess as to what species of fish you might find in the stream at a given time of the year. Field Procedures In the spring, look for amphibian egg masses in slow-moving backwater areas, side channels, and other wetlands associated with the stream and in your reach area. If you can, take a trip to your stream reach on a spring evening to listen for breeding frogs. 65 15th Edition, 2013 FISH AND WILDLIFE SIGNS MAMMALS ANIMAL SCAT: Mammals may be the most challenging to spot, but they often leave behind evidence of their presence. Note any signs of mammals that you see in addition to actual sightings. Signs may be in the form of nibbled plant matter, scat, bones, fur, tracks, trails, nests, burrows or dens. You can use the scat and tracks keys here and in your field kit to help identify these signs. We also have a more detailed animal tracks guidebook in the Streamkeepers office that you can consult. DOGS Note any sign of dogs in or near the creek, and take photos of them if you can. Dogs can eat spawning salmon and should not be left loose to do so. If notified, the Dept. of Fish & Wildlife can investigate and contact the appropriate landowner. RECORDING WHAT YOU FIND Record what you see in the space provided on your data sheet: 1. You can document the species you see, or use broad categories to record your wildlife sightings. For example, birds are categorized into types such as gulls, ducks, sandpipers, passerines (perching birds), raptors, etc. Herps can be easily distinguished as frogs, salamanders, snakes, turtles, etc. 2. Include information on number, size, and activity. Feel free to estimate, using the “~” symbol in front of a number to denote “approximately.” 3. If no fish or wildlife are observed, write “None” in the data boxes. 4. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. Field Procedures 66 15th Edition, 2013 FISH AND WILDLIFE SIGNS FOOTPRINTS (TRACKS)—(note: no turtles on the Olympic Peninsula!) Field Procedures 67 15th Edition, 2013 FISH AND WILDLIFE SIGNS Field Procedures 68 15th Edition, 2013 NOXIOUS WEEDS changed since your last report (new, advancing, or declining weeds), fill out a Noxious Weed Report form (in your team’s EQUIPMENT NEEDED • • • • • • Picture booklet: “Selected Noxious Weeds of Clallam County” Plant identification guidebook Ziplock bag, permanent marker Small shovel, pruners Camera, photo log Noxious Weed Report sheet, clipboard, pencil forms folder). 4. On the Noxious Weed Report, fill out the date, your name, and the site name and brief description. Circle a choice from 1-9 indicating property ownership. Fill in the landowner’s name, when known. 5. Record the width of the reach area surveyed, including the stream area, and the length of reach surveyed along the stream. Noxious weeds are introduced plant species that are aggressive, invasive, and once established, difficult to control. Noxious weeds tend to crowd out native plants, causing environmental damage, economic losses, and even public health and safety problems. State law mandates control of some species. 6. Imagine you were looking down at your reach from the sky; how much of what you see is covered by noxious weeds? (These could be at ground, bush, or tree level.) Indicate category of weed cover: 0-5%; 6-50%; or 51-100%. Complete a Noxious Weed Report at each site that you visit during summer quarterly monitoring, as well as whenever there are new data to report (new, advancing, or declining weeds). Turn in reports along with your other data sheets. This report will go to the Clallam County Noxious Weed Control Board Coordinator. 7. Check the box indicating whether noxious weeds were detected. If the answer is no, skip down to the comment section as desired. 8. If the answer is yes, complete the chart for each weed that you find. For each weed species, first imagine drawing a dotted line encompassing the entire infestation zone of that weed within your survey reach. Estimate the size of that infestation zone (width and length)—if the weed is ubiquitous, the infestation zone may be the same size as your survey reach. Feel free to turn in additional Noxious Weed Reports for any other infestations that you notice in your daily travels. 1. Survey your reach area for noxious weeds. It may help to review the identification booklet before going out in the field, or to ask the Noxious Weed Coordinator (as of June 2012, Cathy Lucero at 360-4172442) what weeds you might find at your sites. If you don’t find the plant in your Noxious Weed booklet, you may find it in the plant identification book. 9. Within that weed’s infestation zone, group together all of that weed’s plants in your mind, then decide on cover class based on the following categories of coverage within that zone: 2. On your Streamkeepers data sheet, indicate whether you’re completing a Report, or if you didn’t check for noxious weeds. Put your complete initials in the “Sampler’s initials” box. 1 – 1-20% 2 – 21-40% 3 – 41-60% 4 – 61-80% 3. If your visit is part of summer quarterly monitoring, or if the weed situation has Field Procedures 5 – 81-100% 69 15th Edition, 2013 NOXIOUS WEEDS possible.) Keep the sample in as good a condition as possible (refrigerating it if you store it temporarily at home, or even putting it in water), and when you return your field kit, turn the bag in to the Noxious Weed Control Office or Cooperative Extension. If you would Estimate as best you can without getting obsessed; if in doubt, consult with your fellow samplers. Remember, your main goal is to report the situation to the Noxious Weed Coordinator. 10. If you find a plant that you would like identified, use the “OTHER” line at the bottom of the survey sheet, and write “Sample #__.” Use a marker to write the date, location, and Sample # on a ziplock bag. Place a complete sample of the unknown plant in the bag, and seal it. (Include leaves, flowers, and roots if like to be notified of the results, include a note with your name and phone number. 11. Take photos if possible, especially if the weeds have advanced or are in bloom. Complete the photo log for each picture. Cover Class General Descriptions Cover Class Definition Imagine drawing a dotted line encompassing the entire infestation zone of that weed species within your survey reach. Within that infestation zone, group together all of that species in your mind, then decide on cover class based on the following categories. 1 1%-20% Present, but less than ¼ of infestation zone covered by that species 2 21%-40% More than ¼ but less than ½ infestation zone covered by that species 3 41-60% About ½ of the infestation zone covered by that species 4 61%-80% More than ½ but less than ¾ of the infestation zone covered by that species 5 81%-100% Between ¾ and 100% of the infestation zone covered by that species Rough Sketches of Cover Classes Field Procedures 70 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING Benthic macroinvertebrates are animals without backbones, such as insects, worms, scuds, and mollusks, which live at the bottom of streams. Our stream teams collect them, and professional labs identify them. However, volunteers are welcome to examine the invertebrates before or after preserving them—see last part of this protocol—and can volunteer to help sort samples. (The June 2012 revision of this protocol is based on new protocols developed by collaboration between the WA Dept. of Ecology and local governments in the Puget Sound region—see Wilhelm, Lester, and Fore, 2011.) EQUIPMENT NEEDED (Items with an * are in the regular bags rather than the “bug bag”): • 95% denatured ethanol (remember to get WHY SAMPLE MACROINVERTEBRATES? The best way to assess the health of a watershed for living things is to look at those living things. Undisturbed watersheds in the Pacific Northwest contain a marvelous variety of benthic macroinvertebrates, representing a smorgasbord of shapes, sizes, survival strategies, and adaptations. Human activities that interfere with natural processes in a watershed have a definite and predictable impact on the types and numbers of invertebrates that live there. Many invertebrates are just as sensitive to changes in their environment as salmon. We tend to be more interested in fish than invertebrates, but there are several good reasons to sample invertebrates rather than or in addition to fish: • It is easier and less intrusive to the environment to sample invertebrates. • Whereas anadromous fish are impacted by a variety of factors such as ocean conditions and fishing pressure, stream invertebrates are primarily impacted by activities within their watershed. • Invertebrates have a wide geographic distribution, making it fairly easy to predict which types should be present where. • Since invertebrates are an important food source for fish (and other wildlife), sampling them measures an environmental component with a direct impact on fish. • Undisturbed streams have such a great variety of invertebrates that sampling can reveal subtle disturbances over space and time. this from the storage cabinet outside the office before taking the field kit home) • • • • • • • • • • • • • • • • • • • • • • • • • • • 1 complete Surber sampler 2 buckets, marked “clean” and “dirty” 2 500-micron sieves, also “clean” and “dirty” 4 rubber dishpans strong weeding fork to disturb substrate “Clean water” decanter with handle 2 angled-spout wash bottles (one for water, one for alcohol) 2 spray bottles (one water, one alcohol) macroinvertebrate handling tools: o plastic spatula o flexible forceps (tweezers) o one rigid forceps o magnifying glasses o lighted magnifier o head magnifier o spoons wide-mouth sample jars with tight lids foam holder for sample jars electrical tape pre-printed labels—outer & inner ziplock bags—small and large 4 weights with flagging tape attached permanent marker macroinvertebrate ID field keys *stick thermometer *reach map or site sketch for each reach *100’ tape *timepiece with second hand *camera *rubber gloves *tarp *data sheet, clipboard, pencil OPTIONAL: extra buckets for sitting OPTIONAL: beach umbrella with stake & sledgehammer for rain Field Procedures NOTE: Please also measure gradient if it has never been measured at your site (see separate protocol). 71 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING HOW DO MACROINVERTEBRATES PROVIDE A “BLOOD TEST” OF A WATERSHED’S HEALTH? invertebrate populations into a generalization about stream health. It is a powerful analytical tool. A wealth of information about the B-IBI is available on the Streamkeepers web site at http://www.clallam.net/streamkeepers/html/bio logical_monitoring.html. We can assess the biological health of a stream by looking at the types of invertebrates that either thrive or do not thrive in it. If only a few types of invertebrates live there, or if the invertebrates are primarily ones that adapt well to disturbed streams, there is some kind of problem present. A group of teachers and students at the University of Washington (later spun off as the nonprofit group SalmonWeb) developed a means to sample invertebrates in a uniform way, identify and count them, and then perform calculations to assess stream health. The calculations measure such things as: • The total variety and balance of life forms present (a.k.a. biodiversity) • The variety of types of mayflies, stoneflies, and caddisflies—invertebrates that form an important part of the diet of salmon and trout, and that respond in complex ways to different human disturbances • The variety or number of invertebrates that are known to adapt very well or very poorly to streams that are unnaturally warm, cloudy, or de-oxygenated • The variety of invertebrates that need clear spaces between rocks or stable habitat for a long time span. By sampling at many sites, both disturbed and undisturbed, these scientists were able to develop a set of calculations that give a good indication of the biological health of streams and their surrounding watersheds. These metrics are known as the Benthic Index of Biological Integrity (B-IBI) for the Puget Sound Lowlands. The macroinvertebrate samples you collect will be professionally identified, and the counts will be entered into a database that calculates the B-IBI for each sampled reach. The B-IBI yields a single number on a scale (much like a test score), along with a description of that number, ranging from Healthy to Critically Impaired (much like a grade on a report card). Thus, the B-IBI enables us to transform information about Field Procedures WHEN TO SAMPLE The Puget Sound local governments have decided that the target sampling window can cover at least August-September. In some circumstances, it may be acceptable to sample a bit after the end of the sampling window if there hasn’t been a big rainfall event; check with staff. Also, check weather reports beforehand: if riffles are more than a foot deep, you can’t see under the water, or conditions are unsafe, don’t collect bugs that day—but you might be able to do your regular water-quality monitoring instead. Generally, you’re less likely to get rained out earlier in the sampling window, so try to schedule early if possible. If you do sample when water levels are up, avoid sampling a riffle that would have been dry before the rain. WHERE TO SAMPLE • • • • 72 The B-IBI we currently use is only calibrated for streams up to a certain size. Consult with staff if you intend to sample a site where bankfull width is >60’. Try to sample at least 165’ upstream or 660’ downstream of a bridge or other large human-made structure (unless you are trying to measure the structure’s impacts). The sample reach will ideally include four distinct riffle habitats (fast, turbulent water moving over gravel or cobble substrate), with two digs from each riffle for a total of 8 digs. If you cannot find four riffles, you can distribute your digs evenly in the available riffles. If there are no riffles anywhere in the vicinity, sample in areas with fast-moving water where the stream is straight and fairly uniform, the water is 412” deep, and the substrate is appropriate (see below). The best substrate would be 2-4” rocks, with smaller pebbles underneath. Avoid 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING sampling in rocks larger than 12” on the surface-layer or larger than 4” below that. • Look for the best overhead canopy and riparian vegetation. • If possible, avoid sites with filamentous algae on the rocks. To try to meet the above conditions, you can range fairly widely from your normal waterquality monitoring location, as long as you: a) Avoid disturbing vegetation overhead or upstream of your sampling site. b) Inspect the Surber sampler netting and collection cup for tears, holes, or critters. Apply duct tape if needed and note problems on data sheet. c) Once in the riffle, place the device quickly to avoid scaring bugs away. Frame out your Surber sampler, and place it on the selected spot with the opening of the nylon net facing upstream and the collection cup stretched out behind. Find a spot where the frame rests as flush as possible with the stream bottom. The current should move directly into the net. If the current is very slow or the water very shallow, take extra precautions to make sure the water is moving all the way down the net and into the cup. You may need to remove rocks or even excavate a little channel downstream of the frame. d) Larger rocks resting within or beneath the frame need to be brushed off carefully, with hands or a brush, to let any bugs on them wash into the net. Stay in an area that has similar gradient, valley shape, and riparian land-cover. • Don’t cross any inputs to or outflows from the stream. • Document your location (explained below). Note that in many cases, you are being asked to sample a site because of its disturbances, so there may, for example, be no true riffles or only fine sediment. In that case, your job is to find the best sampling spot you can there. • NOTE: If your site is less than ideal or simply not appropriate for collecting a sample, explain the situation in the “Comments” section of your data sheet, and take photos illustrating your points. FIELD PROCEDURE Only brush off the part of the rock resting within the sample frame. 1. Overview: Beginning downstream and moving upstream, you will collect eight 1-ft2 digs with the Surber sampler, ideally with two digs in each of four riffles—see diagram below. Sample within the stream’s main flow and avoid the sides and downstream edges of riffles. Within a riffle, you may place the digs side-to-side or back-to-front. Then set the rock aside in the stream, or if the entire rock was within the frame, you can put it in a dishpan for later examination. Once these rocks have been removed, the frame should be squarely on the stream bottom. If you 2. Collect a sample: Field Procedures can’t pry a big rock out, brush it off in place, concentrating on any cracks or 73 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING 3. Transfer the sample to collection jars: indentations, and move the frame as needed to get the back flush with the bottom. Note any problems on your data sheet. At this point, note the water depth in inches on your data sheet, using the marked notches in the Surber’s frame. a) Put a little alcohol in a sample collection jar and put the jar in the foam holder, near the dishpan. b) Examine any large rocks collected in the dishpan, using a magnifying glass. Using a brush or forceps, gently move any organisms found into the sample jar. After examining each rock, spray it with alcohol over the pan or double-check it carefully, then set it on the bank. Clean water can also be used for rinsing rocks and hands. e) Once the larger rocks are removed, disturb the substrate vigorously with the weeding fork for 60 seconds, to a depth of about 4”. (You should dig vigorously enough to be breathing hard). Organisms and detritus should wash into the net. As you dig, watch to keep material from going around the sides. TO MAKE “CLEAN” WATER FOR RINSING: Pour it from the “dirty” bucket, through the “dirty” sieve, into the “clean” bucket. c) When all rocks have been cleaned, pour the water from the dishpan through the clean sieve. Rinse the pan, agitate and pour again. This should filter out any invertebrates that washed off of the rocks. Then return the rocks to the stream in the area of the sampling site. f) If you hit more big rocks while digging, take a “time out” from the 60 seconds to pry them out. Brush off the portion that was within the sample frame and set aside in the stream, or if the entire rock was within the frame, you can put it in a dishpan for later examination. If you can’t pry a big rock out, brush it off in place as above, and note it on your data sheet. STRINGY ALGAE ON THE ROCKS? Scrape off as much as you can with something sharp and collect it all. You may have to get spaghetti jars from home—don’t fill any jar over halfway. d) Meanwhile, the other samplers should attend to the Surber sampler. Wash all objects caught on the inside of the net into the collection cup: g) At 60 seconds, lift the sampler out of the water, keeping the open end pointing upstream and tilting it up out of the water, to help wash organisms into the collection cup. h) Without emptying the cup, repeat the sampling procedure at the next digging spot. Remember to record the water depth with each dig. When you finish digging in a riffle, mark the area of this riffle’s digs with one of the flagged weights, near the center of the dig area. • water so that most of the objects inside wash into the cup. • Finish rinsing the contents of the net into the cup. You may use the “dirty” bucket to pour unfiltered water into the net from the outside, or you may pour filtered (“clean”) water down the sides of the net from the inside. e) When the net is clean, empty the contents of the collection cup into the 2nd dishpan. Clean the neck and collar of the sampler over the dishpan to i) If you can collect all 8 digs without overfilling the Surber’s collection cup, do so. Otherwise, when the collection cup gets nearly full, you’ll need to take a break in sampling and empty it. Field Procedures With the opening out of the water, rotate the net around in the 74 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING mud stuck to it; the mud will later escape through the sieve. collect any critters that may remain inside. Examine the net carefully and pick out any remaining invertebrates, then set it aside. Rinse the cup and empty again, continuing until you have emptied it completely. (To rinse, you may pour clean water inside the cup; or you may dip the cup into the stream, holding it upright, and let the stream water filter in through the mesh on the side of the cup.) i) Put a bit of water back in the dishpan and comb over it with the lighted magnifier (which will get critters to move) and rigid forceps (which will pick them up efficiently). Keep a keen eye out for caddisflies, which in their cases look very much like small rocks, and chironomid tubes, which look like globs of dirt or sand. If you are sure that only rocks and sand are left in the dishpan, discard the contents; if not... f) Large taxa: Pick out any bigger, predatory-looking insects and put them in the sample jar to protect the other ones! Freshwater mussels , which look like ocean mussels with their oblong, fragile-looking shells and are usually of some size, should be pulled out of the sample, counted, noted, photographed, and returned to the stream. In contrast, little “seed” clams no bigger than a pea, crayfish and snails should be included in the sample. Critters still crawling in the sand? Try an “alcohol float”: Decant the water out of the dishpan, then put in enough alcohol to cover. Swirl and see if critters start releasing from the sand particles. If so, decant them into the sieve, catching the alcohol in another dishpan. If there are critters in that waste alcohol too, save that as well, marking it “Thru sieve from alcoholfloat.” If this doesn’t work, collect both sand and critters. g) Pick out non-decayed large debris (sticks that you can’t break easily and leaves that you can hold upright from the stem) from the material in the dishpan. Using a magnifying glass and squirt bottle or tools, remove any organisms to the dishpan or sample jar before discarding these debris pieces. Decayed debris should be collected in the sample because it might hide organisms inside (e.g., if a leaf is limp, damaged, or “skeletonized”). j) Transfer the remaining contents of the clean sieve into the sample jar, which the rock-pickers should have finished with by now. Your job is to get everything that’s now in the sieve into the sample jar, a.s.a.p. Get the contents down at one end to make them easier to remove, by agitating the sieve at an angle in shallow clean water in one of the dishpans (like panning for gold). Use gentle forceps, a spatula, and/or a squirt bottle to move the remaining contents of the clean sieve into the sample jar. (One technique is to squirt alcohol from the back, washing the material along with the alcohol into the cup.) Fill the jar no more than halfway with “stream stuff,” then fill to near the top with alcohol. h) Pour some clean water into the dishpan and swirl the sample around in it. While the water is still agitated, pour it off into the clean sieve. Most of the organic matter should enter the sieve with the water, while the rocks stay at the bottom. Repeat this decanting procedure until the water is completely clear and there are no invertebrates still crawling around in the debris in the dishpan. If you’ve collected a mat of algae, shake this mat to loosen up any Field Procedures k) Now turn the sieve over in a clean dishpan and spray with clean water from the backside to collect any bugs that remain on the sieve. Examine the sieve carefully to make sure there are no 75 15th Edition, 2013 BENTHIC MACROINVERTEBRATE SAMPLING critters left; any still hanging onto or wrapped around the mesh can be removed with a bit of alcohol and the rigid forceps. c) Indicate whether this “riffle” was turbulent or non-turbulent. d) Record this riffle’s width and length to the nearest foot. l) Use a pencil to fill out one of the preprinted internal labels, with the agent, project, site, date, samplers’ initials, jar __ of __, and # of SqFt. Place inside the jar, ideally so that the writing can be seen from the outside. Close the jar tightly (users of “pop-top” jars pay close attention here!) and wrap several times, starting on the lid and then working your way down, concentrating on closing the gap between the lid and the jar. Leave a ½” pull-tab at the end. e) Repeat this procedure for the other riffles. 6. With the flagging and measuring tape still in place, photograph each riffle. A set of photos consists of: m) Use a pencil to fill out one of the preprinted external labels, with the agent, site, jar __ of __, date, # of SqFt , and chief sampler’s initials. Tape to the outside of the jar. • The riffle area itself, ideally showing the measuring tape and some of the substrate. (Find the angle where the light gives the best view.) • The riparian corridor taken up- and downstream from the riffle. Complete the photo log section of your datasheet (see sample below). n) Place all the jars from the site in a single sealed bag, using another external label, this time indicating the total number of jars. (Larger bags are included in the field kit.) 4. If you are not performing Water Chemistry monitoring during this visit, take the air and water temperature, following the protocols outlined in this Handbook. 7. Collect your flagging & measuring tape. 8. In the “Sampler’s Initials” box on the data sheet, put the full initials of the chief sampler taking responsibility for this sample. 5. You now have flagging at each of your riffles. Starting with Riffle #1: 9. If you have been asked to take a replicate sample at this site, take a lunch break first, and rest your eyes and back! Then move upstream in the same reach and repeat the above procedure, indicating “R” after the site name. If you were not given an extra data sheet, hand-write the data on the back of the original data sheet. a) Measure its direction (upstream or downstream) and distance from the zero-transect or reference point of your reach (see Reach Map or Sketch Map protocols), and record that on the data sheet under Dig #1. b) On your data sheet, indicate which other digs were part of this riffle by recording the same Riffle # for them. Field Procedures 10. Clean and store the equipment. Make sure the net and sieves are clean—use the brush in the kit to clean them if needed. 76 15th Edition, 2013 GRAB SAMPLING FOR LAB ANALYSIS (BACTERIA, NUTRIENTS, ETC.) NOTE: Grab sampling is generally accomplished not by regular stream teams, but by a special team that collects a large number of samples in a single day, in what’s known as a “tour” in the Clallam County Water Resources database. The following instructions are based on the WA Dept. Ecology's general sampling SOP (Joy 2006). similar procedures can be used for many other EQUIPMENT NEEDED--GENERAL types of lab analysis. • Field manual Microorganisms, nutrients, metals, etc. are • Data sheets—see “Data Sheets” section naturally present in streams, but humans can • Clipboard, pencils, waterproof marking pen change both the quantity and nature of these • Directions to collection sites • Sterile bottles, one for each site & lab bottle, inputs in a way that upsets nature’s balance: plus replicates/blanks/extras Pathogenic (disease-causing) microorganisms • Timepiece that humans or domestic animals introduce to • Exam gloves water—including varieties of bacteria, viruses, • Thermometer or multimeter and protozoa—can cause diseases in humans • Salinity meter (optional—see below) and animals alike, including salmonella, • Sampling wand to attach bottles to hepatitis, and giardia. • Large cooler to keep in car One way to test for the presence of human• Portable cooler to carry to sites introduced pathogenic microorganisms is to • Gel ice packs or ice focus on fecal coliform bacteria, which primarily • Hand disinfectant live in the digestive systems of warm-blooded • Anti-contamination supplies (see separate animals, aiding digestion. These bacteria, protocol) though not pathogenic themselves, are good SPECIAL EQUIPMENT/INSTRUCTIONS: indicators of human or animal waste The above equipment is standard for fecal contamination, which often carries other more coliform grab samples, the most common type harmful organisms that are harder to test for. collected by Streamkeepers. There are many Hence, Washington State water quality other possible lab analytes; in addition to the standards use fecal coliforms as the indicator of instructions provided here, follow any special potential pathogenic conditions in streams. instructions provided by the lab or project manager. Some items often needed: • • Similarly, excessive inputs of nutrients (forms of nitrogen and phosphorus, delivered to water bodies through fertilizers, livestock, or leaking septic tanks) can lead to Blue Baby Syndrome, reduced livestock vitality, “brown blood disease” in fish, and eutrophication--a massive build-up and die-off of vegetative matter that takes up the available dissolved oxygen in the water and suffocates fish and the macroinvertebrates they depend on. Nutrient loading can be particularly devastating to nearshore marine areas. Field collection bottle, used to fill the lab bottles. Acid-wash before sampling day: rinse with 1 N HCl, then rinse 3X with distilled water and let dry. This bottle can then be used at multiple sites simply by rinsing twice before sampling; however, if a site is particularly contaminated, the collection bottle should be “retired” for the day and a fresh bottle used. Face mask if caustic chemicals are used. When elevated levels of pathogens, nutrients, or other constituents are present, water quality may be at risk, and State Water Quality Standards recognize unacceptable levels of many of these constituents (Washington Administrative Code, Chapter 173-201A). WHY GRAB SAMPLES? Many types of water analysis are exclusively or optimally performed in a laboratory. This protocol describes sampling for bacteria, but Field Procedures 77 15th Edition, 2013 GRAB SAMPLING WHEN TO SAMPLE note that on the tracking sheet and plan your next sample day to avoid such situations! Periodicity: For routine ambient monitoring, Streamkeepers samples quarterly as follows: • • Winter: January • Spring: April or May • Summer: August 1 – September 15 • Fall: October 5 – 31 Special projects may require different scheduling, such as monthly sampling (required for certain State Water Quality Reporting purposes) or storm-based sampling. If there’s no flow: Zero flows can be important data, so if no water is flowing, it’s important to record that fact on your data sheet. Indicate one of the following: ANY proposed sampling date must be confirmed well in advance with the processing laboratory (in Streamkeepers’ case, usually the Clallam County Environmental Health Lab, 360417-2334. NOTE: The lab does not take samples on Fridays.) The lab will generally provide bottles and other required sampling equipment; be sure you also have access to the other equipment listed above. • Creek bed completely dry throughout reach. • Water present in pools, but no apparent flow. • Water present between rocks, but no apparent flow. • Water present, but level and/or velocity are too low to measure with a meter. FIELD REPLICATES: Our quality control plan requires that for 10% of samples, a second sample be collected for a replicate test. Field replicates give an indication of how much variability there is in the equipment, sampling techniques, and environment. Time of day: Ordinarily, bacterial samples must be delivered by 2 p.m. and within 6 hours of the first sample, but some projects may differ; for example, stormwater projects often accept a 24-hour holding time to increase the flexibility of sampling. Stay in close touch with lab managers about expected delivery dates/times. To perform and record field replicates: • Streamkeepers staff or the team leader will determine how many replicate samples need to be collected, select sites for replicates, and then notify team members where they’ll need to collect replicates. • At the replicate site(s), the team will grab a second sample, as soon as possible after the first, and in the same spot. • On the Streamkeepers Sample Tracking Sheet, write “FR” in the “Field Rep?” column on the line for the replicate sample (see sample field sheet at the end of this section). Tidal sites: If you’re supposed to be testing the freshwater runoff of a stream, you need to avoid tidal interference: • • • • Check tide tables (available online) before planning the collection day. Samples taken near the mouths of streams should be taken on an outgoing tide. In general, you can sample ½ hour after mean high tide, defined as the point halfway between the high-low tide and low-high tide for the day. If a salinity meter is available, take it along and sample salinity. Note the reading on the tracking sheet. FIELD BLANKS may also be required: follow the same collection procedure as a regular sample, using distilled water instead of sample water. Be sure that the water is flowing downstream when you sample. If the tide has turned and you notice upsurge effects, Field Procedures Sites that are well above the stream mouth should have no problem with tidal interference. 78 15th Edition, 2013 GRAB SAMPLING FIELD PROCEDURE d. If you’re in water >6” deep, hold the bottle near its base and plunge it below the water surface with the opening pointing downward. Collect the sample 8-12” below the surface, or midway between the bottom and the surface if the water is shallower. Turn the bottle underwater into the current, moving it slightly upstream as you turn it up, and take the bottle out of the water when it is filled up to the shoulder—see figure below. 1. Fill the car cooler with ice or ice packs; the latter are less messy and keep colder longer. 2. Take the portable cooler with you to each site, with enough ice to chill the sample(s) until you get them back to the car cooler. 3. Bottles should be labeled before collecting samples. Fecal coliform collection bottles, if reusable, should be pre-numbered. If there is no number on the bottle, mark it per lab instructions. You may also have to affix tags to the bottles after sampling. 4. Collecting the sample: a. Enter the stream downstream of where you plan to sample, to avoid contaminating the sample from your boots or stirred-up sediment. Sample at a point where the stream is flowing, well mixed, and preferably at least 6” deep. (If there is no such place at your regular site, you may have to go outside it; if so, note your location on the tracking sheet.) Get as far away from the banks as you can. Choose a spot that appears undisturbed and has little or no sediment stirred up in the water, if possible. It is preferable to use a sampling wand, as this stirs up the bottom far less than walking in the creek, and also avoids decontamination problems; see AntiContamination Protocol. b. For a bacterial bottle: uncap the bottle2 and do not let anything touch the inside of the cap. Do not rinse the bottle or cap. If the bottle becomes contaminated (e.g., if you touch the threads or hit it on the stream bottom), discard it. c. For a field-grab bottle: rinse it twice with stream water (as well as its cap) before sampling. 2 If the site has a noticeable layer of “gunk” on top, either take all samples at the site by removing the cap under water, or remark upon the surface layer at that site on the data sheet. Field Procedures 79 15th Edition, 2013 GRAB SAMPLING • If the bottle comes out with the water level below the shoulder, pour out the water and try again. • If the bottle comes out full, quickly flick the bottle until the water level decreases to the shoulder. If more than a few seconds have passed, cap and shake the bottle before flicking. at end of section). The “Sampler in Charge” is the person ultimately responsible for the data at those sites on that day. Be sure to include all initials. 11. At each site, enter on the tracking sheet: a. The bottle number, if there is one. b. The site name; if you do not know its name, describe it well enough that its location is clear. e. If the water is <6” deep, you have a couple of options: • • c. “R” for field replicate or “B” for blank (see discussion above). Sample in shallow, fast-moving water, preferably at a point where the water is forced between a couple of larger rocks. Hold the bottle facing upstream so as to catch the moving water in it. Avoid hitting the bottom. d. The time of sampling. e. Sample collector’s initials. f. Other water-quality measures (e.g., temperature) as instructed. If there is a drop-off somewhere, as from a cascade or culvert, you can sample from this drop-off so long as the bottle touches nothing but the falling water. g. Any noteworthy remarks—e.g., a flock of ducks on the water, abundant leaf litter, strange debris, high turbidity, unusual smells—or problems sampling. 12. If using a field-grab bottle to fill other bottles, rinse this bottle & its cap with distilled water when finished at site. 5. Recap the bottle carefully, without touching the inside. 6. If there is a number on the bottle, record that number on the data sheet. Otherwise, follow instructions for that project. 13. Transfer sample bottles to the car cooler. 14. When finished sampling, bring all samples and forms directly to the laboratory or shipping site. On your data sheet, enter the time that you turned the samples in, and have someone from the laboratory or shipper initial the time that they’ve received the samples. Submit the data sheets that the lab requires, and make copies for the Streamkeepers office. Don’t forget to turn in a Tour Cover sheet and Volunteer Hours sheet for your team. 7. Put the bottle in the cooler, or, if you’re using this bottle as a field-grab bottle to fill laboratory bottles, be sure that anytime you’re pouring or extracting sample from the field-grab bottle, you cap and invert it several times to mix. 8. Follow any additional instructions from the lab, such as filtering or adding fixatives. Gloves and mask may be needed. 9. If this is a site where you are to take a replicate or blank, repeat the sampling procedure. Indicate R or B as instructed on the tracking sheet. 15. The lab will process the samples and submit results to Streamkeepers staff, who will enter the information into the Clallam County Water Resources database and then issue a report. 10. At your first sampling site, fill out the headers on the Tracking Sheet (see example Field Procedures 80 15th Edition, 2013 BANK STABILITY ASSESSMENT To help evaluate the severity of the erosion and revetment you documented in the Erosion/Revetment protocol, this protocol provides a simple rating scale, based on some easilyrecognizable factors. It was developed at the University of Washington [Henshaw and Booth, 2000], and has been found to provide reliable results when the assessments are performed by different observers (R2 = 0.71 indicates a strong correlation between scores given by different observers [Sossa and Booth, 2004]). FIELD PROCEDURE 1. Assess the entire vicinity of your reach, if possible, not just the part within the “official” reach boundaries. By “vicinity,” we mean the entire stretch of stream that has similar characteristics (gradient, valley/channel shape, and riparian vegetation) to your “official” reach. 2. Use the scale below to assess the degree of stability/instability, and check it off on your data sheet. Categories of bank stability, from Henshaw and Booth (2000), adapted by Sossa and Booth (2004), further adapted with assistance from Booth 2004. Class Description 4 STABLE Herbaceous vegetation other than just grasses down to the ordinary low-water line (us. the bottom or “toe” of the bank slope) No raw or undercut banks No recently exposed roots No recent tree falls 3 SLIGHTLY UNSTABLE Vegetation to water line in most places Some scalloping of banks Minor erosion and/or bank undercutting Recently exposed tree roots rare but present 2 MODERATELY UNSTABLE Vegetation to water line spare (mainly scoured or stripped by lateral erosion) Bank held mainly by hard points (trees & boulders), and eroded bank elsewhere Extensive erosion and bank undercutting Recently exposed tree roots and fine root hairs common 1 COMPLETELY UNSTABLE No vegetation (other than grasses) at water line Bank held only by hard points Severe erosion of banks on outside bends and both banks on straight stretches Recently exposed tree roots common Tree falls and/or severely undercut trees common 1 ARMORED BANKS Banks held by placed structures such as riprap, retaining walls, etc. Field Procedures 81 15th Edition, 2013 BANK STABILITY A slightly unstable bank (Class 3): Jimmycomelately 0.6 A moderately unstable bank (Class 2): Jimmycomelately 0.2 prior to channel restoration A completely unstable bank (Class 1): Valley 0.4; note the failed revetment. Field Procedures 82 15th Edition, 2013 EQUIPMENT NEEDED GRADIENT • • • • Sight level (“peashooter”--in leather case) 100’ tape stadia rod data sheet, clipboard, pencil Using this procedure, known as the “peashooter” method, you will measure the downhill slope (gradient) of the water surface. Two people are required: a sighter and a rod-holder. The sighter should ideally be someone with a steady hand and a good eye. A tip: the sight level fogs up in rainy weather, so carry it in your shirt pocket (close to your body) to minimize fogging. 1.45 ft. is at the tip of this line. WHERE TO MEASURE: The ideal place: Reminder that this is still the onefood range (in red) • • • • • is fairly straight and in a single channel, with a good sight line, and with no downstream constrictions that may cause backwater effects during high flows is representative of the section of the creek your reach is in has 2 identical habitat units (e.g., the tops or bottoms of 2 pools or riffles) for endpoints is at least 50-100 feet long is upstream of your cross-section line (if your reach has one) Do the best you can to meet these conditions; you may go outside your reach if necessary. (NOTE: Placement will be different if you are measuring gradient for a stream gage—consult with staff if this is the case.) Tenths (in black) HOW TO MEASURE: Try to have more than one set of samplers perform this procedure (or switch roles) to increase your precision. 1. Decide where the sighter and rod holder will stand. (Who stands u/s & who stands d/s is purely a matter of convenience of reading the height on the rod.) The sighter then takes position in or alongside the stream and sights through the peashooter to where the rod-holder will eventually be, leveling it by getting the bubble in the middle of the 3 lines. Meanwhile, the rod-holder extends the stadia rod from the bottom section until the button clicks, so that the rod reads above 7’, and sets it down next to the end of the peashooter, leveling it by holding it with two fingers from above like a plumb-bob. The rod-holder then measures the “Pupil Reading” on the rod to the middle of the leveled peashooter, to the nearest hundredth of a foot. (See stadia rod picture.) Feet (in red) STADIA ROD The markings are unusual: feet are written in red and tenths in black; each bar is 0.01 ft. thick; the halfway point between tenths is the pointed tip of the longer line in between. Field Procedures 83 15th Edition, 2013 GRADIENT • If you measure with the bottom of the rod right at water level, you can enter a zero for “Correction Factor.” • If the rod is resting below or above the water level (e.g., in the water or on a rock), you need to record the Correction Factor that would need to get added to the Pupil Reading to get the height above the water: o If the rod is resting below the water level, this will be a negative number. o If the rod is resting above the water level, this will be a positive number. centered on the sight level’s center mark. The sighter then determines where the center mark crosses the stadia rod, either by reading the numbers on the rod her/himself, or by giving signals or verbal directions to the rod-holder to move a dark, straight object (such as the sightlevel case) in front of the rod until its top aligns with the center mark. The rod-holder notes that “Sight Reading” to the nearest hundredth of a foot, then measures the Correction Factor if the rod is resting below or above the water level (see previous section), and enters both values on the data sheet. 5. 2. The sighter holds the tape reel while the rodholder takes the rod, the clipboard and pencil, and the end of the tape, and walks to the predetermined point. You may have to do some minor pruning of overhanging branches or walk outside of your reach to get a good sight-line. Run the tape between you along the water. The two then stretch the tape between them, along the contour of the water, and record the “Distance” on the data sheet, to the nearest tenth of a foot. 3. The rod-holder holds the stadia rod at any convenient point (given the criteria stated above), making sure it is straight up by using the “plumb-bob” technique described earlier. 6. If there is no adequate straight stretch, you may have to take multiple straight-segment readings as you go around a bend at the deepest point of the water. If you take an “additive” gradient in this manner, record values for each segment separately and note that the values must be added together, which can be done in the office. 4. The sighter, standing in the same position and posture as in step 1, sights through the sight level (with the label at the top) toward the stadia rod, and adjusts it so that the bubble is 7. In the “Sampler’s Initials” box, put the sighter’s initials next to each set of measurements; record any comments relevant to the quality of each set. Sample gradient data sheet Pupil reading Pupil height correction factor (- if below water level, + if above) 5.21 0 Sight reading Sight height correction factor (- if below water level, + if above) Distance 5.16 -0.24 91.4 Pupil/Sight heights above water = Pupil/Sight readings + correction factors Gradient = “rise/run” = ABS[(pupil height above water)-(sight height above water)]/distance Field Procedures 84 15th Edition, 2013 ESTABLISHING CROSS SECTION MONUMENTS EQUIPMENT NEEDED • • • • • • • • • • • • • • • • CHOOSING A LOCATION FOR THE LINE In most reaches, you will establish a single cross-section line, preferably across a fairly straight and even stretch of stream in a riffle, run, or glide (not in a pool or cascade), where there are no islands with woody vegetation. Midway between bends is ideal. (If your reach has two pool/riffle sequences, you may want to establish two cross-section lines, one in each of the riffles.) Do not put the line across a place where the streambed or banks are bedrock (i.e., you want an “alluvial” rather than a “confined” reach). In exceptional circumstances, you might have to place the line outside of your reach--but it should be near enough to mark on your reach map. reach map from prior monitoring 100’ measuring tape 100’ of string 6” - 8” galvanized nails small sledge hammer hand pruner lengths of 1/2” rebar 2 - 4 feet long rebar caps hardhat safety glasses first aid kit flagging tape line level compass stadia rod clipboard, pencil Consider the following points when establishing your line: In this procedure, you will establish a permanent monument on each bank of the stream from which to measure its crosssectional profile. You will perform this procedure only once: before your first August monitoring session. (If the monuments are removed or disturbed, you will have to reestablish them.) By stretching a string and a measuring tape between the two monuments (using the Cross Section Survey field procedure), teams can take annual measurements that will accurately show changes from year to year. Large changes indicate possible problems in the watershed. • You’ll want a place easy to find again and to put in monuments. • When possible, find two trees (preferably fir) >8” diameter that are on opposite sides of the stream and show no sign of imminently falling. In that case, you can establish monuments simply by driving nails in low on the trunks of the two trees. Where trees are not available, you will have to drive rebar into the ground, ideally leaving about 4” obtruding from ground level. Often one monument will be in a tree and the opposite will be located with rebar. • Attachment points should be well above the level of bankfull flow (see definition in “Bankfull” chapter)—a few feet above is ideal. HOWEVER, the line should be low enough that the stadia rod (14.5 feet as of July 1999) can measure up to it from the lowest point in the channel, and you can accurately read it. Field Procedures 85 15th Edition, 2013 ESTABLISHING CROSS SECTION MARKERS INSTALLING THE MARKERS • The cross-section line should be as perpendicular as possible to the bankfull channel (see definition in “Bankfull” chapter). 1. To decide exactly where to drive nails or rebar, have two people stretch a string between the proposed points, with the line level attached in the middle. BE CAREFUL NOT TO FLIP THE LINE LEVEL OFF THE STRING. Adjust as necessary to make the line level and perpendicular to the channel. • The two monuments need to be easily accessible without damaging the banks. (Otherwise, changes in the channel’s crosssection will be due to the stream teams themselves!) • There must be NO interference with the string. Use the hand pruner to remove branches that are in the way. • If the monument will be a nail in a tree, try to locate the nail on the upstream or downstream side of the tree so that the nail itself is parallel to the channel; however, the most important concern is to make the line perpendicular to the channel. Locate the nail as low in the tree as is practical. • If the monument will be rebar driven into the ground, hold the string about 2 inches above ground level. The person on the other bank should adjust height as necessary. • If there are no trees, put rebar on both banks. • Avoid placing rebar in high-traffic areas, for both safety and the integrity of the markers. • If you place your cross-section line in a good place to measure stream flow, you may be able to combine measurements for both protocols. (Program managers will help you determine if your cross-section line is a good spot to also designate flow measurements.) However, in that case your line must be perpendicular to the stream channel. LOCATING THE MONUMENTS Monuments should ideally be directly across the stream from each other, marking a line that is more-or-less perpendicular to the channel. To determine perpendicularity, first choose a point on either bank where you wish to place your first monument. Stand in the middle of the channel facing this chosen point. Hold your arms out to your sides and shift your feet until your arms line up with the flow. Then bring your hands flat together in front of you. Your hands should be pointing at the chosen marker. If they are not, move your body up- or downstream until they are. Now double check your position by again holding your hands out from your sides and bringing them together in front of you. You will be pointing to the marker along a line that is roughly perpendicular to the flow. Then turn 180 degrees keeping your body in the same place, and repeat the movement with your arms. You will be pointing along the same perpendicular line towards the other bank at the best spot for your second monument. Use this procedure to determine if two trees will work or if you’ll have to place rebar on one or both banks. Field Procedures 2. Before driving nails, make a number of pleats in flagging tape, leaving a 6” tail on the end. Then hammer the nail through the pleats. (This will assure that some flagging will remain if the tail is pulled off.) Try to leave at least 3” of nail protruding. If the nail is not parallel to the channel, bend it with hammer blows near the base until it is, but do not bend the nail head closer than 1” to the tree trunk. The attachment point will be the head of the nail. 3. If driving rebar, use hardhat and safety glasses. Leave at least 4” protruding. Use the two-foot lengths of rebar if possible. If the ground is hard, you can use a piece that has a point ground into it. If the ground is soft, use a longer piece. You can also pound fist-sized rocks into the ground around the rebar to stabilize it. If you cannot drive the rebar any further and it is 86 15th Edition, 2013 ESTABLISHING CROSS SECTION MONUMENTS MARKING THE MONUMENTS secure, you can cut it off at 4” height with the hacksaw. The attachment point will be just below the rebar cap, once installed. If available, label the monuments themselves with metal tags. Include: 4. Test your two attachment points with the string and line level to see if they are secure and level with each other, and adjust if necessary. 5. Install a safety cap on the top of rebar pieces, then use the hacksaw to score the rebar just below the bottom of the cap, thus making a permanent mark for the attachment point for the string. • Site name • LBM or RBM • Distance & azimuth to another landmark at the site (e.g., the other cross-section monument, reach marker, or other landmark) • Instructions as to where to attach the string to the rebar or spike. MEASURING THE DISTANCE RECORDING THE MONUMENTS Use the steel measuring tape to take an accurate measurement of the distance between your monuments, to the nearest 0.1 foot. Get the tape as taut as you can; you may need one or two people pulling on each end. Measure between the designated measuring points on the monuments: Measure the distance from your reach’s zero point to the cross-section line, and record this information on your reach map. Also on your map, indicate the placement of the markers: • For nails in trees, record the approximate position and height on the tree. • For rebar: just below the rebar cap. • For rebar, indicate the approximate position. • For a nail: at the head of the nail. • Also give the distance and true bearings from two prominent landmarks nearby (one of which can be your monument on the other bank). (See “Compass Use” section for instructions on taking a bearings.) That way, if the tree or rebar “disappears” (whether through vandalism, blowdown, or a year’s worth of brush growth), you can relocate or reestablish it. FLAGGING THE MONUMENTS Make it as easy as you can for volunteers to find the markers in future years. You may wish to: • tie flagging around the trunk of the tree at eye level • tie flagging in the brush above your rebar • tie flagging to overhanging vegetation at eye-level in mid-channel near the crosssection line SEE The SAMPLE MAP AT THE END OF THE REACH MAP PROTOCOL – Page 101. However, if the site is frequented by the public, flagging may serve as both a visual nuisance and an invitation to disturb the markers. Use your best judgment. Field Procedures 87 15th Edition, 2013 This page is intentionally blank for printing. Field Procedures 88 15th Edition, 2013 BANKFULL: WHAT IT IS AND HOW TO LOCATE IT WHY BANKFULL? edge, and you should consider all that are present at a given site: Several procedures in this manual require you to locate what is known as the “bankfull channel edge,” or more simply as “bankfull.” This is an important concept in understanding the workings of a stream. 1. Bank slope: In stream channels with natural (undiked) riparian areas and a low, flat floodplain, the bankfull edge is located at the edge of this plain. Often the floodplain will slope down very gradually and then more abruptly. This abrupt slopebreak is usually a good indicator. However, you may find such a slope-break on only one bank, or none at all, for instance if the channel has cut down into the streambed. Or the slope-break may be impossible to find on a bank that is slumping or undercut. 2. Vegetation: The bankfull edge is often indicated by a demarcation line between lower areas that are either bare or have aquatic and annual vegetation, and higher areas with perennial vegetation such as ferns, shrubs, and trees. (Keep in mind, though, that the vegetation line is always in transition, retreating during wetter periods and advancing during dryer ones. So except for ferns, you should rely most heavily on perennial vegetation that is more than 6 feet high.) One particular confusion arises from willow or alder trees growing within the bankfull channel, because the channel has migrated into them, or they fell into the stream and managed to reestablish themselves. Therefore, when you look at vegetation, you should also look at soils… 3. Soils: Look for a transition as you move up the bank, from cobble/gravel to sand/silt to soil. Above bankfull level, you should find old leaf litter forming into soil with organic matter. (Beware: this may be covered by flood deposits, so you may have to dig down.) 4. Point bars and bank undercuts: Often on the inside of meander bends, the stream will build up a bar of sediment from the eddy current created by the bend; the top of such a bar is the minimum height of bankfull. Similarly, on the outside of such bends, the stream will often undercut the bank and expose root mats. If you reach up HOW DOES A “BANKFULL” GET CREATED? Most lower portions of streams in our area are alluvial, meaning that they create their own channels by moving sediment from the surrounding hillslopes and from the stream channel itself. Major episodes of such movement occur during floods and are called “channel-forming events.” These events determine the size of the channel needed to convey the water. In a period of relatively stable climate and land-cover, a stream system will develop equilibrium between its flows and the size of the channel, whereby the channel is large enough to contain the stream under most flow conditions. When flows are greater than this capacity, the stream overflows its banks and flooding occurs. In such streams, the channel is usually big enough to contain a high-flow event that recurs on an average of every 1.5 years (which we call the “1.5-year flood”). Such a frequency of inundation is frequent enough that perennial vegetation can’t grow there, either because its roots are too wet or its seedlings get swept away. So usually, what you’ll see if you look at the cross-section of a stream channel is a sort of “bowl” that contains the stream most of the time, inside which no perennial vegetation grows, and a place over the top of this bowl where the water can flow during a high-water event greater than a 1.5-year flood. This “floodplain” may be on one or both banks, depending on the site. WHAT ARE INDICATORS OF BANKFULL? Most stream systems are in a continual cycle of change, and every site is unique; thus, no single indicator of bankfull can always get you the “right answer.” There are several indicators that can help to identify the bankfull channel Field Procedures 89 15th Edition, 2013 BANKFULL beneath this mat, you can estimate the upper extent of the undercut. This would also be the minimum height of bankfull. 5. Lines on boulders/bedrock: If you’re in a steep channel with no clear floodplain, look for the highest mineral-stain line or the lowest line of lichen or moss on stable rock. 6. Adjacent indicators: If the indicators are unclear where you’re looking, try looking upor downstream to see if there is a clear bankfull line from which you can extrapolate. no longer 100% sure that you’re below bankfull, mark that level with a flag or stick. b) Then walk up to what is clearly dry land, and walk around, observing indicators and moving back toward the bankfull edge. When you’re no longer 100% confident that you’re above bankfull, mark that point. c) Reassess the indicators and your confidence levels, and consult with your fellow samplers, and make adjustments as needed. d) The bankfull channel edge is at the elevation point midway between these two points. 2. Now follow the same procedure on the other bank. If it is not possible to accurately identify the bankfull level on that bank (which often happens on the outside bank of a meander bend), locate it using a level line from the bankfull point on the first bank. HOW SHOULD I LOCATE BANKFULL? The following method was found by the TFW program to maximize data precision and minimize bias toward over- or under-estimation of bankfull elevation: 1. Start on the bank with the best bankfull indicators. a) Move up the bank from the channel, observing the indicators listed above. When you reach a point at which you’re Typical bankfull ID situation, adapted from Pleus and Schuett-Hames, 1998. (Also referenced for this section: Harrelson et al., 1994.) Field Procedures 90 15th Edition, 2013 CROSS SECTION SURVEY EQUIPMENT NEEDED • • • • • • • • • • to make sure your attachment points are at the same elevation. Tie the string in such a way that you can easily untie it without cutting it. It is crucial that the string not touch anything in between the monuments. If necessary, pull or prune away any brush that interferes. Hang a line level at midpoint on the string to confirm that the string is horizontal, but take it off before proceeding. string line level flexible measuring tape marked in tenths of a foot spring clamp(s) stadia rod compass hand pruner “Photos—Summer” protocol directions to the cross-section monuments (hand-drawn reach map, verbal directions, someone who knows) data sheet, clipboard, pencil 4. Starting at either bank, stretch a measuring tape marked in tenths of a foot across the stream between the two monuments. Keep the tape away from the string by attaching it as closely as possible to the tree (if the monument is a nail) or the ground (if the monument is rebar). You can use the piece of wire at the end of the tape to secure the end-hook such that the tape’s zero point is at the head of the nail or the bottom of the rebar cap, or you can wrap the tape around the monument and then clamp it to itself using the spring clamp. (The tape doesn’t have to start at zero.) The tape should be fairly tight, but it will sag below the string, which can be stretched more tightly. Make sure that the tape does not touch the string at any point. In this procedure, you will survey the stream channel cross section with a series of measurements along a permanently-established line. The data you gather will be entered into a computer database that can generate a graph of the cross section and calculate the degree of change in the cross-section “footprint” over time. Survey the cross section at the place in your reach where permanent monuments have been established. Generally there will be one set of two monuments in each reach. The location of these monuments should be indicated on your reach map. See the “Establishing Cross Section Monuments” procedure for further details. 5. Begin readings from either monument (lbm or rbm). You don’t have to begin at zero, and you can start at either end of the tape— the database will make all necessary conversions. One person records on the data sheet while the other measures with the stadia rod. 1. Avoid trampling down the banks, or your own team will be the cause of changes in the cross section! 2. Locate and verify your monuments, and complete the lines on your data sheet describing your monuments and any changes to the site. 6. Assure that the rod is straight up by holding it loosely and finding the point at which it balances itself. Read from the side of the rod that is actually touching the ground (the up-bank side). Be sure to have your eye on level with the string. 3. Tie a string tightly between the attachment points on the two permanent monuments. For a nail in a tree, the attachment point is directly next to the head of the nail. For a piece of rebar in the ground, the attachment point is the scored line in the rebar just below the rebar cap (or just below where the rebar cap would be if the cap is missing). When in doubt, use the line level Field Procedures 7. At the starting point, on your data sheet: • 91 In the “Descr” column, circle whether you’re starting at the lbm or rbm. 15th Edition, 2013 CROSS SECTION SURVEY • In the “d” column, record the reading on the tape (which won’t necessarily be zero), to the nearest tenth of a foot (DO NOT GIVE MEASUREMENTS IN INCHES). • In the “ht” column, record the height on the stadia rod from the ground to the string’s attachment point to the monument—to the nearest tenth of a foot. event that you’d expect to see every couple of years. Generally, if you can kick the rock out of the way, do so, or just skip over the rock if it’s too big for you (but not the water!) to move. However, if the boulder or tree looks like it wouldn’t move during a bankfull flood, count it as part of the channel bed. 12. Undercut bank: If the wetted edge is beneath an undercut bank (or protruding log), act as if the wetted edge were at the edge of the overhang. (See diagram on next page.) When your stadia rod butts up against the overhang, record that distance as your wetted edge. Your vertical measurement should be from the stream bottom to the string, as usual. On your data sheet, record “undercut” next to your wetted-edge designation. You can also record the water depth at that point. (See sample field sheet on next page.) Make measurements 0.1’ on either side of the undercut edge. 8. You do not have to measure at uniform horizontal intervals; in fact, you should not use uniform intervals. Instead, use longer intervals where the slope or terrain is regular, and shorter intervals where it is irregular (such as at the steep drop-off at the edge of the bank). In general, intervals should be 0.2 – 2 ft. when measuring above bankfull (see definition below) and 0.2 – 1.5 ft. when measuring below that line. The person with the stadia rod moves along the cross-section line, measuring from the ground to the string. Two numbers are given at each point: the horizontal reading on the tape measure, and the vertical distance from the ground to the string, both in tenths of a foot. 13. If you wish to provide a double-check on the water level, you can measure the water depth at mid-channel, or at more frequent points if the water-level is not uniform across the channel due to small pools or cascades. Enter these measurements in the “wtr” column. 9. Be sure to stop and measure at the bankfull points (lbfull & rbfull). (See separate “Bankfull” chapter for how to determine these points). Flag these points for the photo-taker, by either a flagged stake or flagging hanging from the tape. 14. Proceed as described above all the way to the monument on the other side. 10. Also stop at the left- and right-bank wetted edges (lbwe & rbwe). If the water level is fairly uniform across your line (which it should be if the monuments were wellplaced), these two vertical measurements should be equal and should reflect the level of the water across the channel. 15. In the space provided on your data sheet, calculate the bankfull width, which you will need to perform the Erosion/Revetment and Pools monitoring protocols. 16. Before taking the tape and string down, perform the “Photos—Summer” protocol. You may also be able to perform the Flow protocol using this tape, if it is not too high for the flow meter’s staff and is at a good point to measure flow (see “Where to Measure” in the Flow protocol). 11. Once you get into the water, ignore any rocks or wood sitting in the bankfull channel that look like they could be moved in a “two-year flood”—the sort of high-flow Field Procedures 92 15th Edition, 2013 CROSS SECTION SURVEY Next measurement will be 0.1’ further along, at top of bank Field Procedures 93 15th Edition, 2013 CROSS SECTION SURVEY Cross-sections, Bear 5.1, 2000-2003 0.00 0.00 distance from rbm 10.00 20.00 30.00 40.00 50.00 60.00 -0.50 -1.00 ground ht. from monuments -1.50 -2.00 -2.50 bankfull Thalweg shifted between 2001 & 2002 -3.00 -3.50 -4.00 -4.50 Major erosional event in the winter of 2001- 2000/130 2001/233 2002/1052 2003/3645 -5.00 d from RBM Field Procedures 94 15th Edition, 2013 LARGE WOODY DEBRIS EQUIPMENT NEEDED • • • • • • 100’ tape, stretched along your baseline retractable tape ruler camera, photo log “Photos—Summer” protocol data sheet, clipboard, pencil WHAT’S BANKFULL, ANYWAY? See the separate chapter on “Bankfull” for details. However, in addition to that chapter, consider this: LWD within the bankfull channel will affect the flow of water at flood stage, so another sign that the LWD is within the bankfull channel is that you’ll see signs of erosion or deposition near the LWD. In this procedure, you will tally, classify, and photograph large pieces of wood that intrude into the stream’s channel along your stream reach. Large woody debris (LWD) enters the stream from the adjacent riparian zone and plays a crucial role in shaping fish habitat. It: • • • • • 2. A living log is a piece of wood that: creates diverse pool/riffle habitat provides cover for fish traps sediment and smaller organic debris such as logs and twigs prevents spawning areas from being inundated with large sediment loads retains organic matter long enough for it to break down and become more appetizing to aquatic invertebrates a) will not die within a year (roots still in contact with soil), but is fallen or tipping; b) is longer than 10 feet and has a diameter of at least 10 inches at the thickest point; AND c) intrudes into the bankfull channel (see definition), even if it’s only the rootwad portion. Definitions 3. A rootwad is a piece of wood that: We define 4 categories of LWD: a) does not qualify as a log; 1. A dead/dying log is a piece of wood that: b) has a root system at least 3 feet in diameter; a) is dead or will die within a year; b) is no longer supported by its own roots; c) has a diameter of at least 10 inches at the base of the stem where it meets the roots; c) is longer than 10 feet and has a diameter of at least 10 inches at the thickest point; AND d) has roots that are detached from their original position; AND e) intrudes into the bankfull channel. d) intrudes into the bankfull channel (see sidebar). Field Procedures 4. A logjam is an accumulation of 5 qualifying logs or rootwads that are in contact with one another or associated with the same structure, intruding into the bankfull channel by at least 4 inches. If you count a logjam, do not tally the individual logs/rootwads. 95 15th Edition, 2013 LARGE WOODY DEBRIS However, there are exceptions to the above guidelines. For example, a log or a rootwad may be partially buried in the bank, so you may not be able to see its full size. If simple attempts to jostle it are unsuccessful, and if it appears to be functioning to trap sediment and debris, or to create pools or bars, then it qualifies as a log or a rootwad even if the dimension criteria aren’t apparent. As a local habitat guru once said: “If it’s performing the functions of LWD, it probably is LWD!” 3. After tallying, write out and circle the total number in each box. Remember to write zeroes if none is observed. Don’t leave any box blank! 4. If there are any pieces that don’t meet the criteria above but nevertheless seem to be serving channel-forming or habitatcreating functions, note them on your data sheet. (One example would be undercut tree roots that overhang the creek, thus creating cover and acting as a hydraulic control during floods.) FIELD PROCEDURE 1. For each LWD piece of any type, tally on your data sheet the number of pieces by category and zone of lowest intrusion. The zones are defined as: 5. Take photos of the LWD pieces, using the “Photos—Summer” protocol. 6. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data, even if you wrote zeroes in all the boxes. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. a) The wetted channel (the wet part of the stream!) on the day you are monitoring. b) The bankfull channel (see previous sidebar), if the LWD does not intrude into the water. 2. If you can tell that some of the LWD has been installed as part of a restoration project, rather than having been recruited naturally, make tallies in 2 separate subcolumns: “natural” and “artificial.” Field Procedures 96 15th Edition, 2013 EROSION/REVETMENT SURVEY EQUIPMENT NEEDED • • • • • Revetment refers to any action taken by humans to make a streambank more resistant to erosion. A typical revetment consists of a blanket of large “riprap” rocks, but revetment may also consist of wooden or concrete bulkheads, log cribbing, cabled trees, revegetation, and a number of other technologies. Both erosion and revetment are signs of bank instability and can present a number of problems to fish (see inset below). 100’ tape, stretched along your baseline bankfull width calculation from CrossSection data sheet “Summer Photos” protocol camera, photo log data sheet, clipboard, pencil Erosion is the wearing-away of the land surface by water or wind. Here we refer specifically to the erosion of stream banks. WHAT’S ALL THE FUSS ABOUT EROSION & REVETMENT? A diverse mix of mature riparian vegetation growing on the banks of a stream indicates that the banks are relatively stable. An undercut bank, if well-vegetated, can still be stable and provide excellent protective habitat for fish. A certain amount of scouring or erosion generally occurs on the outside bend of stream meanders, where water velocity is greatest. In this survey, you are looking for signs of unstable banks, erosion beyond that caused by natural forces, and human intervention to stabilize the banks. A stream bank with little or no vegetation usually indicates that excessive bank erosion is occurring. Signs of erosion include rills and gullies cut by runoff flowing down the banks into the stream channel. Sloughing or collapsing banks are another obvious sign of erosion. Unstable bank undercuts threaten fish habitat, as they are highly prone to sloughing. Armoring banks with rock or concrete may remedy emergency erosion problems. However, artificial bank stabilization tends to deflect and concentrate the force of stream flow downstream to unprotected areas. Thus, forcing a stream into an unnatural humanpreferred course may accelerate erosion downstream. It also limits the stream’s ability to create a natural diversity of habitats. For this reason, you need to look for and note any signs of artificial bank stabilization. (Adapted from Murdoch et al., 1996.) Field Procedures 97 15th Edition, 2013 EROSION/REVETMENT SURVEY FIELD PROCEDURE 4. For revetted areas, indicate: 1. Walk your reach, looking carefully for places where the bank has either eroded or been revetted. a) the approximate length (in feet) of the revetment which lies within the monitoring reach 2. Only record eroded areas that reach bankfull height and are at least two bankfull-widths long. (See your cross-section data for your bankfull width.) b) the type of revetment (check all that apply): i) continuous blanket -- layer of rock, tires, etc. on the stream bank 3. For eroded areas, indicate: ii) bulkhead -- retaining wall made of wood, steel, or concrete a) the approximate length (in feet) of the eroded area which lies within the monitoring reach iii) spur dike -- structure that juts out into the stream b) the highest height of the eroded area, in feet iv) check dam -- low structure crossing the stream c) the probable cause of the erosion (check all that seem to apply): v) large woody debris placement – trees placed, cabled, or dug into the banks or streambed i) slope failure from above ii) bank undercutting by the stream channel, i.e., where the sides of the bank have been dug out by the force of the water and the bank collapsed above the undercut vi) bioengineering -- vegetation planted to protect the bank vii) other - old car bodies, etc. Describe on the data sheet. 5. Take photos of eroded and revetted areas, following the “Photos—Summer” protocol. iii) channel scour, i.e., where the channel has dug the bed of the stream down lower and lower, until the bank has collapsed because its abutment is gone 6. If there are no eroded or revetted areas, write “None” on the data sheet. 7. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data, even if all you wrote was “None.” If more than one person worked on this data, put the initials of the person with the most experience or knowledge. iv) new-fallen large woody debris v) human-made bank alteration upstream or on opposite bank vi) other (indicate) Field Procedures 98 15th Edition, 2013 POOLS SURVEY EQUIPMENT NEEDED • • • at which the calm water begins to accelerate. Look for a narrowing tongue of calm pool water that runs down the middle or side of the stream on the downstream end of the pool. The apex of that tongue should be the deepest part of the outlet. stadia rod bankfull width calculation from cross-section data sheet data sheet, clipboard, pencil 1. During your Cross Section Survey, you determined the bankfull width of your reach. Find your bankfull width on the following chart to determine the minimum residual pool depth for your reach (from SchuettHames et al., TFW 1994): BANKFULL WIDTH MINIMUM RESIDUAL POOL DEPTH 0-8.2’ (ft.) 0.3’ (ft.) 8.2-16.4’ 0.7’ 16.4-32.8’ 0.8’ 32.8-49.2’ 1.0’ 49.2-65.6’ 1.2’ >65.6’ 1.3’ The pool’s residual depth is the difference between these two depths. 4. If the pool qualifies according to the above criteria, write its residual depth to the nearest tenth of a foot on your data sheet. 5. For each pool, record pool-forming factors. Keep in mind that pools form in two ways: a. Obstructions can dam the stream and form a pool upstream of the dam. b. Objects or channel features can direct the water flow in such a way that it scours out the stream bottom in a certain place. Such scour pools are formed and maintained during highwater events, when the stream has a great deal of energy to move sediment. If you visualize these high-water events, you’ll often be able to surmise what created a scour pool. 2. Walk along your reach with the stadia rod, looking for possible pools. These will be areas with deeper water and slower current. (Pools partially within your reach will still count.) 6. On your data sheet, check off as many of these pool-forming factors as apply: 3. If you find a possible pool, determine whether it has the minimum residual pool depth that you determined above. Residual depth is the level of water that would be in the pool if the water level were so low that water wasn’t running out of it any more. To measure it, you need two measurements (see accompanying diagrams): a. Instream wood: A piece of wood can dam the water upstream of it; cause turbulence downstream that digs out a pool; or do both. b. Instream rocks or exposed bedrock: Same as instream wood. c. Roots of standing trees or stumps: Can cause the stream to dig out an area underneath or downstream. a. the maximum depth, which won’t necessarily be in the middle of the pool (estimate the maximum depth if the pool is too deep to fully access); and d. Outside of bend: Greater hydraulic energy at the outsides of bends can dig pools out of the bank. b. the pool’s outlet depth, taken at deepest point of the crest or obstruction that forms the pool’s downstream outlet. The downstream end of the pool is the point Field Procedures e. Resistant banks upstream (may be rock, clay or armored): Can “bounce” high99 15th Edition, 2013 POOLS SURVEY current energy downstream to dig out a pool elsewhere. f. Beaver dam: Uncommon, but obvious when they occur. g. Other/Unknown: Describe possible poolforming factors if you can. 7. If there are no pools, write ”None” on the data sheet. 8. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data, even if all you wrote was “None.” If more than one person worked on this data, put the initials of the person with the most experience or knowledge. Field Procedures 100 15th Edition, 2013 PEBBLE COUNT (From Kondolf 1997, Wolman 1954, and Schuett-Hames et al. 1994) dry when you do your sampling; that just makes it easier to count! EQUIPMENT NEEDED: • • • • Rulers marked in “half-phi” classes (see below), with 1/8” welding rods projecting 8” beyond the end of the ruler latex disposable gloves, to protect against sharp objects in the water marked boot tips data sheet, clipboard, pencil 3. Walk heel-to-toe straight across this channel. With each step, insert the weldingrod straight down to the stream-bottom along the line drawn at the tip of your boots. In this procedure, you will measure the particle size distribution of the surface sediment of your stream, which provides valuable information about its habitat and hydrology. 4. Don’t count bedrock, garbage, construction debris, or organic materials. If you come to an area of the channel that is bedrock only, skip over that area and move to an area with sediment (see #1 above). 5. Otherwise, measure whatever you first touch with the welding rod, be it silt, gravel, or a boulder. It is best for two people to perform this procedure: one to pick and measure rocks exclusively; and the other to record. A second counter cuts the time in half, but the counters must coordinate their crossings (see below). 6. If you hit fine sediment that covers a rock completely (not sporadically), count the fines, not the rock. You can tell if you’ve hit fines, because the rod will make a “scrunch” (sand/silt) or “squish” (mud”) sound rather than a “thunk” (rock) or “thud” (rock covered by algae). You can confirm this fact in a couple of ways: 1. If possible, do your sampling in the area of your cross-section transect. However, the site needs to be a channel-spanning riffle or run3, at a point where the flow and streambottom appear relatively homogeneous (e.g., no eddies or backwaters). If the cross-section transect is not appropriate, find a place that is. You may go outside your reach to find the best place possible if there is no appropriate area within it. (If you see broken glass or other dangerous trash in this area, take precautions, remove the trash, or find another area.) On your data sheet, indicate your sampling location. a) Look for a plume of dirt that flows downstream after you lift up the rod. b) If you’re not sure whether what covers the rock is silt or algae, jiggle the rock, and if the covering easily washes away, it is fine sediment, not algae. 2. The counter(s) will be walking back and forth within this riffle/run across the entire channel bottom where the stream runs during normal flows, from the foot (a.k.a. “toe”) of one bank to the foot of the other. Often there is a non-woody vegetation line at this toe. Part of this area will probably be 7. If you’ve hit fine sediment, you don’t need to pick it up. Just call out “fines,” and the recorder will enter a tally in the “<4 mm” row. 3 Riffle = shallow area where water flows swiftly over gravel and rock, creating surface turbulence; run = area with little surface turbulence but relatively high velocity. Don’t sample at pools or “glides” (places of deep, uniform-depth, slow-moving water). Field Procedures 101 15th Edition, 2013 PEBBLE COUNT Otherwise, pick up the first piece you hit, and measure its diameter along its intermediate axis, which is perpendicular to the other two. To find this, first find the longest axis; then find the smallest axis that is perpendicular to the longest axis. There is now one more axis that is perpendicular to both the longest and shortest axes--that is the intermediate axis. See diagram below. B= Intermediate Axis—this is the axis to measure! they increase by the square root of two and mimic data collected by putting sediment through successively finer sieves.) b) one in the “Total tally” row, to keep track of how many pieces you’ve counted. The recorder should verbally repeat each measurement back to the caller for error checking before placing the tally mark. 10. Repeat this procedure, walking heel-to-toe and crossing back and forth across the riffle. (It will go fast once you get into the rhythm!) Don’t walk back along the same line you’ve walked before! (See diagram below.) flo w shadow (From Schuett-Hames et al., 1994) 8. If you can’t easily remove the rock from the bed, excavate around it and measure it in place. (You may have to “let the dust clear” for a few seconds.) The intermediate axis will be the smaller of the two exposed axes. (If it’s a big rock, don’t give yourself a hernia! Estimate whether it’s embedded or not—i.e., does it look like just the “tip of the iceberg”?) You will tally these pieces in the “Embedded” column on your data sheet (see below). 9. For each piece of sediment measured, make two tallies on your data sheet: a) one in the appropriate row for the piece’s size class, in either the “Loose” or “Embedded” column (not both!). The classes are: < 4 mm; 4-5.7 mm; 5.7-8 mm; 8-11.3 mm; 11.3-16 mm; 16-22.6 mm; 22.6-32 mm; 32-45.3 mm; 45.3-64 mm; 64-90.5 mm; 90.5-128 mm; 128181 mm; 181-256 mm; 256-362 mm; 362-512 mm; >512 mm. (These increments are called “half-phi” classes; Field Procedures 102 General transect scheme for pebble 11. Ifcount you are on a big boulder and the next step is still on the same rock, tally that rock again. 12. If your foot falls on a rock that you can’t stand on, put your foot on top of it and keep your weight on the other foot while you reach down with the rod. If you have to move your forward foot for whatever reason, try to make your next step start from wherever your forward foot would have been. 13. When 100 tallies are reached, all samplers must complete their crossing to the other side of the channel. So if you have a 100-ft. channel and two counters, one should start on each side, and they should meet in the middle! 14. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. 15th Edition, 2013 CANOPY CLOSURE (SINGLE POINT) EQUIPMENT NEEDED • • • you and at elbow height. Identify a rock in the channel directly below the densiometer. Throughout this entire procedure, the densiometer should remain above this rock! The top of your forehead should be visible in the mirror but not the grid area. Close one eye and get your sighting eye in line with the grid centerline. Make sure the densiometer is level by getting the bubble inside of the circle. You will have a “fish-eye” view of the riparian canopy cover. Maintain this spherical densiometer (in small wooden box) knowledge of cross-section transect for your reach (from reach map, written instructions, or verbal directions) data sheet, clipboard, pencil Perform this procedure in January and August. Comparing the two annual readings will give some idea of the amount of cover that is provided by conifers, since the deciduous trees will lose their leaves by January. Do not perform this procedure in January if flows are too high for you to be safe. position while you count. 4. There are four dots in each square of the grid. Count either the dots that are more than half shaded or less than half shaded, depending on which is easier to count. (See sample diagram.) Count systematically, from top row to bottom row, left to right. Anything in the upper canopy that shades the dots counts as 1. Generally, you’ll take this reading along your cross-section transect (or, if there is no cross section at your site, the site’s central monitoring point), in the middle of the bankfull channel (see “Bankfull” chapter). However, you want your reading to be representative of your reach, so if that spot is not representative, move to another spot and note where you moved to on your data sheet. (E.g., if the reach is treeless except for one tree that happens to be directly above your crosssection transect, move at least partially away from that spot.) 2. Your goal is to measure the upper-story tree canopy, not bushy streamside vegetation. If the latter gets in your way of viewing upper-story canopy cover through the densiometer, you may: • Sample spherical densiometer reading. try to ignore the understory blockages when you take your readings; or • cut away a small amount of brush; or • move your location by up to six feet, as long as you remain in the wetted channel. The above example shows 48 shaded points. shade, including tree stems and branches. 5. Record the number of shaded dots on your data sheet in the box marked ”Dn”. If you counted unshaded dots, subtract that number from 96. If you ignored brush or moved location, note that on your data sheet. 6. Interference factors: 3. Face downstream & open the densiometer. Hold it about 12” in front of Field Procedures a) Sun glare: Block the reflection using a finger on your free hand. 103 15th Edition, 2013 CANOPY CLOSURE (SINGLE-POINT) b) Wind in the branches: Try to make your count between gusts. If this is not possible, use your best judgment. readings again, and average them on your data sheet. 9. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. 7. Repeat this procedure facing toward the right bank, upstream, and left bank, turning 90° each time, keeping the densiometer in the same spot and rotating your body around it—remember the rock you identified. (“Left bank” and “right bank” are your left and right while facing downstream.) Record the number of shaded dots for each direction in the boxes marked “RB”, “Up”, and “LB”. 10. The database will calculate the % shade, but if you want to calculate it yourself, add the four numbers and multiply by 0.26. 8. If possible, have someone else or the same person take the canopy closure Field Procedures 104 15th Edition, 2013 CANOPY TYPE PERCENTAGES (REACH-WIDE) (Source: Freudenthal, 1999) EQUIPMENT NEEDED • • reach map data sheet, clipboard, pencil In this procedure you’ll estimate how much of your reach is under the cover of trees, both coniferous and deciduous. This is done in August, when the deciduous trees have leafed out. 1. Visualize your entire reach, consulting your reach map. (It may help to be in the middle of the reach or to walk the channel.) Look at the overstory canopy cover (the highest level of tree branches) in this area, and imagine that you were looking down on this canopy from an airplane. You would possibly see sections of conifer canopy, sections of deciduous canopy, and sections of no canopy (where you can see right down to the ground or bushes). Field Procedures 105 2. Imagining this view from the sky (see sample drawings on next page). Estimate the percentage of your entire reach area over which the canopy is covered by conifer trees, in one of the following three classes: 0-5%; 6-50%; 51-100%. Mark the appropriate class on the “Conifer” line on your data sheet. 3. Do the same for deciduous trees, marking the appropriate class on the “Deciduous” line on your data sheet. 4. If there is a portion of your reach that is not under tree cover, your percentages will not add up to 100%. See the examples below for guidance. 5. If in doubt, consult your fellow team members. Have them make their own estimates before sharing yours. 6. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. 15th Edition, 2013 CANOPY TYPE PERCENTAGES (REACH-WIDE) reach length reach width reach length reach width Field Procedures 106 15th Edition, 2013 CONIFER STEM COUNT (Source: Freudenthal 1999) EQUIPMENT NEEDED: • reach map to determine reach boundaries • 3 measuring tapes • string • flagging • stakes • data sheet, clipboard, pencil stakes, to clearly indicate the “bottom” end of the reach. (You may have to secure the tape on either bank of the stream to keep it from getting dragged in the water.) Repeat this procedure at the far end of the baseline to establish the “top” end of the reach. Then, if possible, connect the corners in the lengthwise direction using another measuring tape, a string line, etc. That way you will have your reach borders clearly marked out. You will count conifer stems, no matter what size or species. (You can generally stop counting at 61 stems.4) Perform this count in January (because the brush is down then!), once every 5 years or whenever there are significant changes in your reach. Three to six people can conduct this count most efficiently. At some reaches where the stream is not safe to cross in the winter, only the “near” bank will be designated for a conifer stem count; this should be clearly indicated on the reach map. 1. Establish the boundaries of your 100’ x 100’ reach, using your reach map to guide you (see Reach Map protocol). If these corners don’t have permanent markers, you will want to temporarily mark them with flagging or stakes. To do this, have one person stand at the zero-point of your baseline with a compass and the reach map. Sight in a direction perpendicular to your baseline, and send two people off in either direction along this “zero transect,” with flagging tape, stakes, and either end of a measuring tape. Direct them as they walk out to their corners, where they will place flags. (See diagram.) If possible, leave the tape along the ground and wrap the ends around the dogleg corners (Count here as well) baseline 3. If you don’t have the outside boundaries laid out with a tape or string, flag them by having two people start at adjacent corners and call out or signal while walking toward each other, flagging along the way. 4 If your reach is larger than a 100’ X 100’ square, your “top-count” number will need to increase proportionately. For example, if your reach is 200’ X 200’, your top-count number will be 241 (because your reach is 4 times larger than the standard reach, and 60 X 4 = 240). However, if you are monitoring a stream with a wide channel that takes up a large portion of the reach, you may have to adjust your top-count accordingly. When in doubt, consult Streamkeepers staff or just count them all! Field Procedures 2. If your reach is not square, you will need to mark the dogleg corners as well. This gets a bit tricky, as the following diagram indicates: (see next page) 4. Have two people stand at either corner on one side of the stream. 107 15th Edition, 2013 CONIFER STEM COUNT 5. Walk toward each other, zig-zagging as needed to cover the area between the stream and your outside boundary line. Count all the living conifers in this area, no matter what size or species, until you meet and have counted all the conifers on one side of the stream (unless there are more than 60 stems—see below). Person 1 starts here stream Persons 1 & 2 finish here 6. Repeat this procedure on the other side of the stream (unless you only count conifers on one bank at that reach, or you have counted more than 60 conifers already—see below). Or, with four people, you can cover both sides of the stream at the same time. (same on this side) Person 2 starts here 7. Once you reach 61 stems, you can stop counting.1 8. Total your count and enter the number (or “>60” if there are more than 60 stems5) on your data sheet. If there are no conifer stems, enter a zero. 9. In the “Sampler’s Initials” box to the right of the data boxes, put all the initials of one sampler taking responsibility for the data, even if all you wrote was a zero. If more than one person worked on this data, put the initials of the person with the most experience or knowledge. 5 If your top-count is greater than 61, change what you write on the data sheet accordingly. In the example from Footnote 2, if you reached 241 trees, you’d write “>241” on the data sheet. Field Procedures 108 15th Edition, 2013 a. A description of your proposed stream/sites/projects and the benefits of carrying out your proposal; SAMPLING PLAN DESIGN HOW TO PROPOSE A NEW STREAM, REACH, OR PROJECT b. List of prospective team members (name, address, phone); Streamkeepers has a regular quarterly monitoring plan that has been devised in consultation with our technical advisors and volunteers. That plan provides a general framework for the ambient monitoring of a stream, meaning that it’s designed to establish baseline conditions, compare conditions between sites and streams, and track trends. Beyond our regular quarterly monitoring, we also perform special projects at the request of partner agencies, volunteers, or other area residents. Each fall, Streamkeepers staff, volunteers and technical advisors work together to determine the streams, monitoring reaches, and projects to be monitored the following year. If you are interested in a stream, site, or project that is not on this year’s work plan, we suggest you do the following: c. If your proposal involves anything other than the regular Streamkeepers quarterly monitoring plan, you’ll need to compose a more detailed sampling plan. We can provide you with reference materials for designing such a plan (e.g., Murdoch et al. 1996 and Yates 1988). d. Contact information for any professionals with whom you’ve consulted (name, agency, address, email and phone number); e. Rationale for your choice of sites, and maps showing those sites. 5. Participate in the Volunteer Advisory Committee and Steering Committee in the fall, and advocate for your stream/reaches. You will advocate most effectively if you are prepared with the aforementioned proposal! 1. Join an existing stream team for the time being. This way you will receive the training and learn our protocols. You can tell Streamkeepers staff which of the existing teams you’d like to join, or staff can assign you to a team. 2. Do the homework necessary to determine the value of monitoring the new stream or reaches, and to locate where the monitoring reaches should be (see “New Reach Establishment” section). You’ll probably want to convene a meeting and/or field trip for local experts to advise you. We can help you get in touch with these experts. 3. Round up a team of volunteers, if possible. Recruit your friends and neighbors! 4. Write an informal proposal showing the results of the above efforts. This doesn’t have to be formal or fancy, but it should include: Field Procedures 109 15th Edition, 2013 SAMPLING PLAN DESIGN CRITERIA FOR SELECTING MONITORING SITES ALONG A STREAM Streamkeepers generally monitors small- to medium-sized wadeable streams, most of which arise in the foothills and are of relatively short length—often just a few miles. In streams we monitor, we generally try to establish three or more reaches: ideally, one at or near the mouth, one or more in developed areas, and one above most/all of the developed areas. This arrangement allows some comparison between stream characteristics at different elevations and levels of human impact. The exact location of a monitoring reach will depend on characteristics specific to each creek (including access, owner permission, creek history, etc.) Resources that can help you identify the most effective and accessible places to establish new reaches include USGS quad maps, driving/walking tours (but don’t trespass), your personal knowledge of the area, and especially the suggestions of local natural resource specialists (Clallam County; Tribes; Clallam Conservation District; State Departments of Fish and Wildlife, Natural Resources, and Ecology; US Forest Service, National Park Service, Natural Resources Conservation Service; etc.). 7. Containing both pools and riffles, if possible. 8. Above saltwater and tidal influence. 9. Generally located at least one half mile apart. 10. If you’re trying to establish a “reference site” which approximates pristine conditions, find a site with little/no adjacent land use, good riparian cover and channel complexity (including pools and riffles), and that’s neither totally incised nor a Devil’s Club swamp! Once you’ve determined where your sites should be and have gotten approval for the new project and sites, you’ll need to establish the new sites by following our “New Site/Reach Establishment” protocol (next section in the Volunteer Handbook) Criteria for selecting reaches to monitor on a given creek include: 1. Reasonable and safe access by volunteers. 2. Publicly owned land or permission of landowner to access and mark sites. 3. A good spot to gather data, either because: 4. It provides a representative view of the stream at that point in its watershed, or 5. There’s a particular land-use impact that you’re trying to track, in which case you’ll want sites both upstream and downstream of that land use. 6. At least 165’ upstream or 660’ downstream of bank alterations such as bridges, riprap, etc., if possible. (Unless your purpose is to measure the effects of these bank alterations!) Field Procedures 110 15th Edition, 2013 NEW SITE/REACH ESTABLISHMENT Here are some steps to go through if you’re establishing a new monitoring site or reach. A “site” is a fairly-contained spot, whereas a “reach” is a specified length of stream; generally, a “site” will suffice unless you’ll be doing physical-habitat measurements, in which case you’ll need to establish a “reach.” For the purposes of this section, we’ll use the words interchangeably. 1. Identify prospective monitoring reaches you think it’s a good idea to diverge from the standard suite. a. Using the resources and criteria described in “Monitoring Program Design,” select prospective monitoring reaches and mark them on a map. b. Use the County Assessor’s maps to identify the parcel number and look up the owner’s name (either at the Assessor’s office or online at http://www.clallam.net/Maps). c. Confirm accessibility of the site through a visit or a drive-by. If private property, contact the owner regarding access. Streamkeepers staff can supply you with a permission form for establishing a monitoring site and a standard letter asking for permission, which you can bring to the owner; or we can mail these items to them at your request. d. Write a brief text (1-2 paragraphs) describing the reach, its location, how to access it, and why you’ve chosen it. If you consulted with anyone, be sure to list his or her name, title and contact information. Also, if you want to do something other than monitor the regular suite of parameters (e.g. you think you should monitor only chemical water quality, or only riparian vegetation, etc.), list the parameters you want to monitor and (briefly) why Field Procedures 2. Confirm selection of monitoring reach(es) with Streamkeepers staff 3. Document and mark the reach a. Complete as much of the “New Site Questionnaire” (see following pages) as you can prior to going into the field. You can get this form from our office or our website. b. Go to the site(s) and: i) Finish the “New Site Questionnaire” ii) Perform the “Sampling Site Sketch Map” or “Reach Map” protocol, depending on directions from program staff. iii) Install monuments and flagging as needed at your reach(es), per the above protocols. c. Draw your map(s), per the above protocols. d. Determine the Washington Department of Fish & Wildlife stream number for each reach; you’ll need the state Water Resources Inventory Area (WRIA) catalog, available from Streamkeepers staff. e. Have staff create a field-forms folder and hanging file for the stream-team, and an office binder for the stream if new. In the binder, include photocopies of maps with the monitoring site(s) clearly marked. 111 15th Edition, 2013 NEW SITE/REACH ESTABLISHMENT STREAMKEEPERS OF CLALLAM COUNTY—NEW SITE QUESTIONNAIRE Dear Streamkeeper advisor/partner/volunteer: You have suggested a new Streamkeepers monitoring site. (For more information, see http://www.clallam.net/streamkeepers/assets/applets/SamplingPlanDesign.pdf&http://www.clallam.net/streamkeepers/ assets/applets/NewReachEst.pdf.) In order to facilitate our addition of this site into our database system, please answer the following questions about each new site you wish to see monitored, using a separate form for each site. You may submit responses electronically or by hard-copy. 1. Your name (and agency if applicable): 2. Brief descriptive name of this site, and stream-mile to the nearest tenth if you can calculate it from a map: 3. Would you like this site sampled quarterly, or only in certain seasons? For what parameters and duration? 4. Where, exactly, would you like this site to be? (Describe in terms of landmarks and rough distances and directions from them.) Please note: Streamkeepers’ macroinvertebrate-sampling protocol specifies that collection sites are to be at least 660’ downstream or at least 165’ upstream of any human-made structure in the bankfull channel, such as a culvert or bridge, UNLESS your goal is to sample the impacts of the structure. So if you think macroinvertebrate samples will someday be taken at this location, follow the above guidelines. 5. Supply good written directions as to how to access this site: 6. Every new site needs to be visited by SK staff or a technical advisor prior to any monitoring. Has this site been visited, and if so, by whom and when? If not, who will be visiting this site, and when? 7. The technical advisor should help decide if flow will be measured at this site, and if so, if it should be measured along a transect between permanent monuments. If so, have the monuments been installed, or is there a plan to install them? (If so, the installation should be indicated and referenced on the Site Sketch Map.) 8. Is it safe to measure flow at or near that site in all conditions? 9. Who owns the site and the access route to it? What are the parcel numbers? (See below for map link.) 10. Have you obtained permission to access these parcels? If so, when, and who did you talk to (incl. phone #)? If not, can you help us make the necessary contacts? 11. Would there be any special access instructions, such as gated access points or the need to contact the landowner prior to each site visit? 12. Is past data available at that site? If so, who/what/when/where & how can we access it? 13. How soon would you ideally like Streamkeepers to start monitoring? (The quicker & better the information you provide, the sooner we can start.) (See next two pages ) Field Procedures 110 15th Edition, 2013 NEW SITE/REACH ESTABLISHMENT LOCATION INFORMATION We need to record accurate information about the locations of all of our sites. Please help us with the following information, to the best of your ability. 14. Horizontal location information: a. Put a dot for this site on an attached map (preferably 1:3000 or larger scale; easy-to-use interactive County maps are available at http://10.5.10.73/aimsiwebsite/arcims_start.htm), OR give a lat/long, preferably in decimal degrees (i.e., set your GPS to read out in this form). b. We also need to know how you placed your dot or took your GPS reading, so please answer the questions below. We need this information in order to share our data with the State and other agencies. Some of the notes in italics should help you with your answers. Horizontal collection method (select one): address match--block face conversion from STR address match--house # digital or manual raw photo extraction address match--unknown digitized--CTR screen/digital data [if located on a computer map without the aid of an air or orthophoto] digitized--paper map air photo--rectified GPS carrier/geodetic air photo--unknown air photo--unrectified cadastral survey GPS code/geodetic GPS kinematic GPS unknown [if you used a GPS and can’t place it in one of the above 3 categories] hand measured--paper map interpolation [e.g., County road maps or USGS 7.5’ quads] LIDAR [e.g., if you used LIDAR hillshade to determine where the stream & site were] address match--street centerline census block 1990 centroid census block group 1990 centroid LORAN-C orthophoto—digital [e.g., Clallam County GIS] orthophoto--paper satellite imagery--Landsat MSS (multispectral scan) satellite imagery--Landsat TM (thematic mapper) satellite imagery--other satellite imagery--SPOT panchromatic satellite imagery--SPOT multi-spectral zip code centroid unknown Horizontal datum (select one): N. American Datum 1927 (NAD27) [e.g., USGS 7.5’quads or NOAA charts] N. American Datum 1983 (NAD83 or 91 Adj.)[e.g., Clallam County GIS] HARN GPS WGS84 (GPS NAVS88) unknown Horizontal accuracy (use your best judgment and select one): <0.01m =>0.1m <1m +-20ft(6m) +-100ft(35m) +-250ft =>0.01m <0.1m +-10ft(3m) +-40ft(12m) +-180ft(55m) +-500ft Field Procedures 111 +-1000ft +-2000ft >2000ft unknown 15th Edition, 2013 NEW SITE/REACH ESTABLISHMENT 15. Vertical location information: a. Provide an elevation in feet: ___________________ b. Provide the appropriate metadata for your answer to the above question, in each table below. Some of the notes in italics should help you with your answers. Vertical collection method (select one): bathymetric sounding GPS (code/geodetic) cadastral survey GPS (carrier/geodetic) digital elevation model[e.g., GPS (kinematic) DEM from Clallam Cty GIS] GPS (unknown) hand measured, paper other engineering survey map[e.g., USGS 7.5’ quads] LIDAR [e.g., using LIDAR 50’ photogrammetry contours] map-derived Unknown Vertical reference (select one): mean sea level mean high high level mean low low highest tide level[DEM from Clallam County GIS, or USGS 7.5’ quads] mean high level mean low level local tide datum mean (half) tide Vertical datum (select one): N. American Vertical datum of 1988 (NAVD88) N. American Geodedic Vertical datum of 1929 (NGVD29)[DEM from Clallam County GIS, or USGS 7.5’ quads] unknown[incl. LIDAR] GPS WGS84 (GPS NAVD88)[e.g., LIDAR] unknown Vertical accuracy (use your best judgment and select one): <0.01m =>0.1m <1m +-20ft(6m) +-100ft(35m) +-250ft =>0.01m <0.1m +-10ft(3m) +-40ft(12m) +-180ft(55m) +-500ft Field Procedures lowest tide 112 +-1000ft +-2000ft >2000ft unknown 15th Edition, 2013 SAMPLING SITE SKETCH MAP EQUIPMENT NEEDED • • • • • • • • pencils with erasers paper (pref. Rite-in-the-Rain; in a pinch, you can use the back of a data sheet) clipboard tape measure sighting compass flagging tape permanent marker If you’re installing permanent monuments, you’ll need the Reach Establishment Kit including: rebar & caps, spikes, sledgehammer, hacksaw, helmet, and goggles. This procedure will guide you in drawing a simple sketch map which will help you document the location of a “point” sampling site (where, for instance, only water chemistry and flow are measured). This map will allow you and others to be consistent in sampling the same spot. Once you’ve created this sketch, a copy will be filed in your stream’s binder in the Streamkeepers office, and another copy will stay in your team’s forms folder, so you’ll be able to refer to it or make revisions as necessary each time you visit your reach. (If you do make revisions, please let staff know so they can change the copy in the office’s stream binder.) This sketch is easy!: Your goal here is just to get the information down, so straight lines, scale, and “compass trueness” are not important in the sketch, as long as you get the proper information across. NOTE: In the instructions that follow, measurements follow the “lay of the land.” So if you’re measuring up a hill, you extend the tape going up the hill rather than on a level. 1. Decide roughly where your sampling site will be; see “Identify Prospective Monitoring Reaches” in the New Reach Establishment protocol. If possible, make the sampling site a place that will be easy for you and others to find and access. Field Procedures 2. Complete as much of the “New Site Questionnaire” as you can before going out in the field. 3. At your site, decide on a “zero-point,” an easily identified point near where your monitoring will occur, and to which exact sampling locations can be referenced (such as when you collect macroinvertebrates). Ideally this will be a prominent landmark which you can flag and draw on your map, such as a big conifer, boulder, bridge, fence post, or end of a path. Otherwise, you can install a piece of capped rebar. 4. At the top of your sketch, include: • • • • • Site name, which in general is the name of the stream plus the stream-miles to the nearest tenth (but see staff regarding exceptions) Date you surveyed for the map First initials and last names of all map sketchers An approximate North arrow Approximate elevation in feet, which you should already have determined while completing the New Site Questionnaire (see New Reach Establishment protocol) 5. Draw a rough map or write directions explaining where to park, and then how to walk to the site from the parking place. Include approximate distances and compass directions as needed. 6. If not prohibited, place some kind of marker near the sampling site. Capped and flagged rebar is best (materials available at the office), or else flagging hanging from a nearby tree or bush. Mark the flagging with your site name and give instructions for getting from the flagging to the central sampling point, if it’s not directly across from the flagging. Try to minimize the visual pollution from the flagging, and yet make sure it’s visible. Usually you can find a branch nearby to hang it from. 7. On your sketch map, reference the samplingpoint to two prominent nearby landmarks, as 113 15th Edition, 2013 SAMPLING SITE SKETCH MAP well as your monument/ flagging. Distances and directions (even approximate) are helpful. explain where the monument is in relation to the flagging. Include on your map: a) The flow-monitoring monuments, indicated as “flow lbm” or “flow rbm”, and as “rebar” or “nail in tree.” b) Distances and azimuths (see “Compass Use” protocol) to each monument from the landmarks described above in #6. 8. Draw the stream on your sketch and indicate the direction of its flow. 9. If all measurements (e.g., flow and water chemistry) are being taken within 50 feet of the identified sampling point, that’s exact enough. If they’re further apart than that (for instance, if the best spot to measure flow is more than 100 feet downstream of the best spot to measure water chemistry), mark each sampling point separately. 11. Sketch any other information you deem useful about the stream and riparian areas. Include observations about such features as vegetation types and locations, 10. Install permanent flow-monitoring monuments if you have been instructed toto so (see New Site Questionnaire and Flow protocol). These will be either rebar driven solidly into the ground above bankfull and sawed off as necessary, or spikes driven into trees. Label these monuments with flagging marked “flow lbm/rbm” to help distinguish them from the brush. If you can’t put the flagging on the monument itself, hang it nearby and Field Procedures 114 15th Edition, 2013 REACH MAP (Note: You only need to draw this map if you are monitoring physical habitat parameters at your site. As of 2005, these parameters are optional, pending further research and discussion among Streamkeepers staff, technical advisors, and volunteers.) EQUIPMENT NEEDED • • • • • • • • • • • • • • • • years thereafter, or as needed (for instance, if there is a major change in the reach). Once you have created a map, the original will be filed in your stream’s binder in the Streamkeepers office, and you will be given a duplicate on which to document any changes that have occurred, each time you visit your reach. pencils with erasers graph paper ruler protractor clipboard marker with permanent ink 3 tape measures, 100-200’, marked in tenths of a foot sighting compass flagging tape stakes big nails rebar rebar caps (required on rebar) small sledge hammer hardhat and safety glasses (to use with sledge hammer) first aid kit Scale: Ideally, use a scale that will fit your entire reach on one sheet of 8.5 x 11 inch graph paper, leaving a ½” margin on all sides. One inch to twelve or fifteen feet usually works well. Draw out a scale bar on the map with increment distances marked, so that the scale can still be measured if the map changes size in duplication. For an example of this scale bar as well as other map features, see the sample map that follows. NOTE: In the instructions that follow, measurements follow the “lay of the land.” So if you’re measuring up a hill, you extend the tape going up the hill rather than on a level. Therefore, if your reach is hilly, your reach map will not truly reflect the plan (overhead) view of the reach. At this stage, full-blown surveying is a luxury we can’t afford! This procedure will guide you in drawing a stream reach map, which will help you document the location and path of the stream channel, various features of the channel and riparian area (area on either side of the stream), and important sampling information. The reach map will help you to replicate sampling procedures and track changes in the stream and riparian area. OPTION: LARGER REACH DIMENSIONS It is also an essential component in continuity of knowledge about your monitoring reach; as you compose this map, keep in mind that all those things you have up in your head won’t do Streamkeepers any good if you get run over by the proverbial bus! A Streamkeepers monitoring reach is typically a 100 x 100 foot square area roughly straddling the stream (with exceptions that we will deal with later.) The central spine of this 100’ square reach is a 100’-long baseline extending along the stream. The instructions below are written as if all reaches are 100’ by 100’, but you may wish to make your reach longer or wider than 100’. For instance, a broad stream may require a 150’ wide reach to even minimally reflect its riparian area, and a reach that is 200’ long might do a better job of reflecting the habitat diversity along the stream. Any reach size is okay as long as it is mapped accurately. Feel free to consult on this issue with Streamkeepers staff or local biologists. Obviously, larger reaches take longer to map and survey; consider the extra time required when making a decision. You will make a reach map when first establishing your reach and then every 3-5 Field Procedures 115 15th Edition, 2013 REACH MAP 1. Decide where your reach will be; see “Identify Prospective Monitoring Reaches” in the Reach Establishment protocol. 2. Next, decide where your baseline will run. Typically, this will be a 100’ straight line that stays close to the stream. If possible, locate both ends or at least the beginning-point at or near some fairly stable and prominent landscape feature, such as a big tree, stump, or signpost. 3. The beginning-point (“zero-point”) of the baseline should be the end easiest for other people to find, following only your map and written instructions. This may be either the upstream or downstream end. If both ends are easy to find, choose the end easiest to access. If safe and permitted to do so, place a flagged stake, rebar (which must be capped), or else just flagging, at the zeropoint. Mark the flagging, “zero point.” In areas that receive foot traffic, keep in mind that: a) Stakes are liable to get pulled out. b) Stakes and rebar might present a safety hazard. c) Markers can mar the beauty of a natural area. d) Weigh these factors in as best you can. 4. Run a measuring tape from the zero-point in the direction you want your baseline to go. Try to keep it close to the stream. It is okay to cross the stream one or more times. If there is a fairly straight trail or road that parallels the stream, you can use it to set up your baseline. This will make mapping easier. 5. If the stream bends such that no straight line can stay within 20 feet of it, make a dogleg in the baseline. Mark that point with a flag and/or stake if appropriate. Then dogleg the tape until you reach the 100-foot point. 6. Draw your baseline on your map as a vertical line, using the scale you have predetermined. Standing at your zero-point, Field Procedures 116 take a bearing to the endpoint or dogleg (see “Compass Use” directions following this protocol), and record the true azimuth (“true azimuth” = the compass bearing corrected to true north, on a 0-360° scale) to the nearest degree on your map alongside your baseline. (If your baseline doglegs, you will have to record more than one azimuth and use the compass to draw the dogleg at the proper angle on your graph paper. You may need to produce a cleaned-up version at home, using a protractor. To make scaling easier, it may be easier to tape a second piece of graph paper onto the first at the appropriate angle.) Clearly mark on your map the zeropoint, the number of feet along the baseline at which doglegs occur (to the nearest tenth of a foot), the 100’ point, and true azimuths of all lines. 7. Reference the zero-point of your baseline to two prominent nearby landmarks. Draw and describe the landmarks on your map, and record both the distance and true azimuth from the landmark to the zero-point. If the zero-point is at one of the landmarks (much preferred!), simply indicate what the landmark is on your map. For example, you may want to draw and write “stake for zeropoint at edge of 6-foot diameter cedar stump, at 20° true from center of stump.” 8. From the zero-point, extend another 100’ measuring tape perpendicular to your baseline. Use the compass to orient this tape correctly. (Simply add 90° to your baseline’s azimuth.) Such a line, perpendicular to the baseline, is called a transect. Normally, you will put the middle of the 100’ transect at the baseline, so that the baseline bisects the 100’ x 100’ outline of your reach. However, feel free to offset the placement of the baseline within the square if that would make the reach more evenly straddle both sides of the stream. For example, if your baseline runs about 20’ to the right of the stream, you could have the transects cross the baseline at the 70’ rather than the 50’ mark. If possible, 15th Edition, 2013 REACH MAP monument or flag the two ends of this transect, which constitute two of the corners of the reach. Mark the flagging as appropriate. 9. Along this transect, measure the distance from the baseline to each wetted edge of the stream (the points where the water surface hits the banks). Record these distances on your map, and mark an "X" on the map at the locations where the transect crosses a wetted edge. dogleg corners 10. Do the same as above with bankfull width (see definition in the Large Woody Debris protocol). baseline 11. Sketch as much information as you can about the stream and riparian areas in the vicinity of this transect. Include observations about such features as vegetation types and locations, pools and riffles, gravel bars, downed logs, and human alterations. Indicate whether these features are measured to scale for location and size. 12. Now move the transect-tape up the baseline at 10- or 20-foot intervals, keeping its intersection with the baseline perpendicular and at the same number of feet that it was for the zero-foot transect. If appropriate, use stakes or flag vegetation to mark the location of the transect lines along the baseline, and mark the flagging as “10’ transect,” etc. If these markers are not visible from the creek, place additional markers on the bank along the transect line—these markers will prove helpful in subsequent monitoring sessions. Mark distances and wetted edges on your map as above, and draw in any landmarks or prominent vegetation that occur near the ends of your transect lines. 13. If your reach doglegs, your reach shape will not be a nice square. Instead, it will have two or more rectangles that overlap each other. On one side, there will be a wedge-shaped piece of gap between the rectangles. If possible, close this gap by extending the outside lines of the two rectangles until they intersect, and make Field Procedures this a single outside corner (see diagram). On the other side, there will be a wedgeshaped overlap between the two rectangles. Eliminate this overlap by establishing a single inside corner where the two outside lines intersect (see diagram). 117 Monument or flag any inside or outside corners if possible—it will enable you to much more easily determine the boundaries of your reach while in the field. And make very clear on your map exactly what the outside lines of your reach are. 14. When you have done the above for all transects, draw the wetted stream by making a curve of the wetted-edge "Xs," and draw the bankfull channel by doing the same with the bankfull “Xs.” Draw the boundaries of the reach by connecting the corners with straight dotted lines. Label all of these lines clearly. 15. You’ll probably want to use the rough map you drew in the field to draw a more precise map at home, with straight lines, proper angles, legible handwriting, etc. For this, you’ll need more graph paper, a protractor, and a ruler, preferably with a strip of the graph paper pasted to it so you can measure distance-increments easily. 15th Edition, 2013 REACH MAP BE SURE THAT YOU HAVE THE FOLLOWING ITEMS ON YOUR MAPS: • Site name (stream name plus the number of stream-miles to the zero-point of your reach, to the nearest tenth) • Date you surveyed for the map • First initials and last names of all map authors • Exact outside boundaries of the reach, drawn in straight dotted lines • Baseline clearly drawn and marked as such • Zero-point of baseline marked and labeled • References to zero-point from two landmarks; these references consist of both a distance and a true azimuth from the landmark to the zero-point. The landmarks should be drawn in and described. • • • If the baseline doglegs, the distance(s) along the baseline at which the dogleg(s) occur, plus the true azimuths of the doglegged lines. The angles between the doglegged lines must be accurate on your reach map; use a protractor or compass to get the angles right. • A legend, consisting of: • • A scale, ticked off like a ruler with map dimensions. Do not put in text such as “One inch equals 20 feet,” because dimensions may change when pages get photocopied! • A true north arrow, clearly marked. The elevation to the nearest 100’, or more precisely if you can. • The cross-section monuments, indicated as “lbm” or “rbm” (left- and right-bank monuments—see protocol on establishing monuments), and as “rebar” or “nail in tree.” • References to each monument from one or preferably two landmarks—same procedure as for landmarking the zero-point, see above. • The cross-section line as a dotted line, with the true azimuth clearly indicated. IF PERMANENT FLOW-MONITORING MARKERS HAVE BEEN INSTALLED AT YOUR REACH (see “Flow”), ALSO INCLUDE ON YOUR MAP: Wetted edges of the stream drawn in as curvy lines. Arrow marked “Flow.” • AFTER INSTALLING CROSS-SECTION MONUMENTS AT YOUR REACH (see “Establishing Cross-Section Monuments”), ALSO INCLUDE ON YOUR MAP: True azimuth of baseline, written alongside the baseline as “__° true.” • AFTER COMPLETING THE “REACH ESTABLISHMENT” PROCEDURE (previous section in this manual), ALSO INCLUDE ON YOUR MAP: • The flow-monitoring monuments, indicated as “flow lbm” or “flow rbm”, and as “rebar” or “nail in tree.” • References to each monument from one or preferably two landmarks—same procedure as for landmarking the zero-point, see above. Features of the stream and riparian areas in your reach: vegetation types and locations, pools and riffles, gravel bars, downed logs, human alterations, etc. Field Procedures 118 15th Edition, 2013 REACH MAP SAMPLE REACH MAP (The original will be filed in your stream’s binder in the office, and you will receive a copy on waterproof paper to take into the field with you.) Flow lbm, rebar, 18’ @ 97° from end-point rebar Flow rbm, rebar, 42’ @ 235° from big cedar Field Procedures 119 15th Edition, 2013
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