Considerations for GHG quantification and assessment of mitigation practices on saltaffected soils Keith Paustian Dept. of Soil and Crop Science Colorado State University Colombo, Sri Lanka 2014 What do you need for effective inventory and assessment? 1. 2. What are the GHG sources and sinks that matter? Understanding of the processes involved a. b. 3. Generalize your understanding in the form of a model a. b. 4. What are the controlling factors, how do they interact, what are the main sources of variability? Both theoretical and empirical (i.e., field studies) knowledge Empirical or process-based, existing or new Validate your model for the circumstances of interest Apply the model for the area/circumstances of interest a. Need the data on the controlling factors (i.e., climate, soil condition, management practices GHG Sources and Sinks Soil C stock change (integrated net CO2 flux) Biomass C stock change ( “ “ “ ) Nitrous oxide emissions Methane emissions (net to the atmosphere) Methane production Methane oxidation Soil C flux processes CO2 Photosynthesis & respiration CO2 Manure Harvest CO2 Litterfall Decomposition & respiration Soil deposition Soil erosion Humification DOC & DIC Controls on soil C stocks C inputs from plant residues and organic amendments f (NPP, dry matter partitioning) f (species, light, temperature, water, nutrients, pest/diseases, salinity, etc. f (how much is left on the field) f (how much is brought in from the outside – e.g., compost, biochar) C losses through decomposition f (microbial activity) f (litter quality, temperature, moisture, nutrients, salinity, etc) f (physio-chemical stabilization processes in soils) f (soil texture, mineralogy, soil structure, disturbance (tillage) Measuring net CO2 emissions/removals from soils Micromet approaches – Eddy Covariance Soil C stock change method • Repeated measures over time • Chronosequences (‘space for time substitution’) Mitigation practices for soil C sequestration Depleting Soil Organic Matter Erosion Intensive tillage CO2 Residue removal Soil organic matter Low Productivity Rebuilding Soil Organic Matter Conservation tillage Conservation buffers CO2 Cover crops Soil organic matter Set-aside Improved rotations Soil C – managing the ‘Input’ side (I) and the ‘Output’ side (R) High residue yielding crops (I) Growing perennial grasses and legumes (I, R) No-tillage and other conservation tillage (R) Cover crops (I, R) Manure additions (I) Reduced frequency of bare fallow (I, R) Other practices that increase C added to soils (e.g., irrigation, improved fertility) (I) Rewetting (flooding) of organic (i.e., peat) soils (R) Tree planting on annual cropland (I, R) Restoration of highly degraded soils (I) Microbial-mediated transformations of inorganic N Anaerobic process Aerobic process Key Points • Chamber design and materials • Deployment time, #gas samples • Time of day • Sampling frequency, # of chambers • Minimum detectable flux • Temporal integration of fluxes • ….and more Flow diagram for DAYCENT. ‘Leaky pipe’ model N2O, NOx NO3- Org. N NH4+ Davidson & Firestone IPCC default model (2006) Direct N2O emissions = 1.0% * N added to soil N added to soil from: •N fertilizer •N fixation (legumes) •Manure/sludge •Crop residues Empirical model based on strip-trials at 6 Michigan farms over 3 years Millar et al. 2010 N2O Mitigation principles Maximize plant use of added N! Improved timing and application rates Reducing N2O Improved placement N2O + Water and fertilizer mgmt NH4 SOM N NO3 Plant N Nitrification inhibitors/ slow release fertilizer N2O Mitigation principles Maximize plant use of added N! IPNI’s four ‘rights’ Right amount Right timing Right placement Right product Robertson and Vitousek 2009 CAST 2004 Soil CH4 flux processes CAST 2004 Mitigating rice CH4 emissions Water management Provide intermittent drainage Organic matter additions Incorporate fresh residues well in advance of flooding Compost residues before applying Use cultivars with reduced CH4 transport Nutrient mgmt – e.g. sulfate containing fertilizer, calcium carbide additions
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