أﻧﻈﻤﺔ ﺗﺼﻨﻴﻒ اﻟﻜﺘﻞ اﻟﺼﺨﺮﻳﺔ-:ًﺧﺎﻣﺴﺎ Rock Mass Classification Systems :ﻣﻤﻴﺰات ﻫﺬا اﻟﺘﺼﻨﻴﻒ Intact Rock and Discontinuity ﻫﻮ ﻧﻈﺎم ﺧﻠﻴﻂ وﻫﺠﻴﻦ ﻣﻦ اﻟﺨﻮاص اﻟﻬﻨﺪﺳﻴﺔ-١ . ﻳﻌﺘﻤﺪ اﻟﺘﺼﻨﻴﻒ ﻋﻠﻰ أﻛﺜﺮ ﻣﻦ ﻣﻌﻴﺎر ﻫﻨﺪﺳﻲ و ﺟﻴﻮﻟﻮﺟﻲ-٢ . ﺗﻜﻮن ﻧﺘﻴﺠﺔ اﻟﺘﺼﻨﻴﻒ ﻣﻔﻬﻮﻣﺔ ﻟﻠﻤﻬﻨﺪس و اﻟﺠﻴﻮﻟﻮﺟﻴﻴﻦ ﻋﻠﻰ ﺣﺪ ﺳﻮاء-٣ ﺗﻢ ﺗﻄﺒﻴﻖ ﻫﺬه اﻟﺘﺼﻨﻴﻔﺎت ﻋﻠﻰ ﻣﺸﺎرﻳﻊ ﻋﺪﻳﺪة ﺑﻨﺠﺎح ﺣﻴﺚ ﻛﺎن ﻣﻦ أﻫﻢ ﻫﺬه اﻟﺘﻄﺒﻴﻘﺎت ﻋﻠﻰ-٤ .اﻷﻧﻔﺎق واﻟﻤﻨﺤﺪرات اﻟﺼﺨﺮﻳﺔ و اﻷﺳﺎﺳﺎت .ً اﻷﻧﻈﻤﺔ ﻣﺘﻔﻖ ﻋﻠﻴﻬﺎ ﻋﺎﻟﻤﻴﺎ-٥ Rock Mass Classification Systems )ﺃ( ﻃﺮﻕ ﺗﺼﻨﻴﻒ ﺍﻟﻜﺘﻞ ﺍﻟﺼﺨﺮﻳﺔ 1- Rock Mass Rating System (RMR - System) By Bieniawski, (1974 – 1989) Using Table Depend on 5 parameters: - Strength - Rock Quality Designation (RQD, %) - Spacing of joint - Condition of Discontinuity - Ground water 2- Quality Index System (Q - System) By Barton, Lien and Lunde, (1974) Using Equation. Depend on 6 parameters: - Rock Quality Designation - Joint set number - Joint roughness number - Joint alteration number - Joint water reduction number - Stress reduction factor (RQD, %) (J n) (J r) (J a) (Jw) (SRF) . ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ- ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض- ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ/د .9 ﻣﻦ١ ﺻﻔﺤﺔ ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر 1- RMR-System )Rock Mass Rating System By Bieniawski (1974 – 1989 ﻴﻌﺘﻤﺩ ﺍﻟﺘﺼﻨﻴﻑ ﻋﻠﻰ ﺨﻤﺱ ﻋﻭﺍﻤل: 1- Strength )2- Rock Quality Designation, (RQD 3- Spacing of Joint 4- Condition of Discontinuity 5- Ground Water د /ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ -ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض -ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ. ﺻﻔﺤﺔ ٢ﻣﻦ .9 ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر ﻟﻬﺎ اﻟﺨﻮاص اﻟﻬﻨﺪﺳﻴﺔ اﻟﺘﺎﻟﻴﺔGranite ﻛﺘﻠﺔ ﺻﺨﺮﻳﺔ ﻣﻦ اﻟﺠﺮاﻧﻴﺖ-:ﻣﺜﺎل Parameter Values UCS 120 MPa RQD 90% Spacing of Joints Condition of Discontinuities Ground Water 1.5 m Very Rough, No separation, Hard wall Wet RMR value Rating 12 20 + 17 =18.5 2 15 30 7 82.5 % :اﻟﺘﺼﻨﻴﻒ و اﻟﻮﺻﻒ The rock mass of Granite is classified as a very good quality of class (I) according to RMR classification system by Bieniawiski, (1989). . ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ- ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض- ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ/د .9 ﻣﻦ٣ ﺻﻔﺤﺔ ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر 2- Q-System Quality Index System By: Barton and others 1974 : ﻳﻌﺘﻤﺪ ﻋﻠﻰ ﺳﺖ ﻋﻮاﻣﻞ 1. 2. 3. 4. 5. 6. RQD%, Joint Set No., Jn Joint Roughness, Jr Joint Alteration, Ja Joint Water, Jw Stress Reduction Factor, SRF Q= RQD Jr . Jn Ja . Jw SRF Classification of Rock Masses according to Q-Values . ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ- ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض- ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ/د .9 ﻣﻦ٤ ﺻﻔﺤﺔ ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر د /ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ -ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض -ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ. ﺻﻔﺤﺔ ٥ﻣﻦ .9 ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر د /ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ -ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض -ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ. ﺻﻔﺤﺔ ٦ﻣﻦ .9 ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر د /ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ -ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض -ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ. ﺻﻔﺤﺔ ٧ﻣﻦ .9 ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر ﻟﻬﺎ اﻟﺨﻮاص اﻟﻬﻨﺪﺳﻴﺔ اﻟﺘﺎﻟﻴﺔShale ﻛﺘﻠﺔ ﺻﺨﺮﻳﺔ ﻣﻦ اﻟﻄﻔﻞ-:ﻣﺜﺎل RQD = 88%, SRF = Near Surface, 3 Sets of Joints, Rough surface Filled with Sand, Wet Joints. /اﻟﺤﻞ Q = RQD . Jr . Jw Jn Q= ( 88 ) 90 * (1) 4 * ( 0.5 ) 2.5 Ja SRF = 0.48 :اﻟﺘﺼﻨﻴﻒ و اﻟﻮﺻﻒ The rock mass of Shale is classified as a very poor quality according to Q-System by Barton and others, (1974). . ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ- ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض- ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ/د .9 ﻣﻦ٨ ﺻﻔﺤﺔ ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر )ﺏ( ﺍﻟﻌﻼﻗﺔ ﺒﻴﻥ ﻨﻅﺎﻡ RMRﻭ Q ﺘﻡ ﺍﻴﺠﺎﺩ ﺍﻟﻌﻼﻗﺔ ﺒﻴﻥ ﺍﻟﻨﻅﺎﻤﻴﻥ ﺒﺎﻟﻘﺎﻨﻭﻥ ﺍﻟﺘﺎﻟﻲ-: RMR= 9 * Ln Q+44 ﻭ ﺫﻟـﻙ ﻤـﻥ ﺨـﻼل ﺍﻟﻌﻼﻗﺔ ﺍﻟﺨﻁﻴﺔ )ﻓﻲ ﺍﻟﺭﺴﻡ ﺍﻟﻤﺭﻓﻕ( ﻤﻥ ﺩﺭﺍﺴﺎﺕ ﻋﻠﻰ ﺍﻟﻁﺒﻴﻌﺔ ﻟﻜﺘل ﺼـﺨﺭﻴﺔ ﻤﺨـﺘﻠﻔﺔ ﺍﻷﻨـﻭﺍﻉ ﻭ ﺍﻟﺘﺭﻜﻴـﺒﺎﺕ ﺍﻟﺠﻴﻭﻟﻭﺠﻴﺔ ﻭ ﺩﺭﺠﺎﺕ ﺍﻟﺘﺠﻭﻴﺔ ﻭ ﻤﺨﺘﻠﻔﺔ ﻓﻲ ﺍﻟﺨﻭﺍﺹ ﺍﻟﻬﻨﺩﺴﻴﺔ ﻤﻥ ﻤﺨﺘﻠﻑ ﻤﻨﺎﻁﻕ ﺍﻟﻌﺎﻟﻡ. ﻭﻟﻬﺎ ﻗﻴﻡ ﻋﻠﻴﺎ ﻤﻥ ﺍﻟﻘﺎﻨﻭﻥ ﺍﻟﺘﺎﻟﻲ-: RMR= 9 * Ln Q+62 ﻭﻗﻴﻡ ﺴﻔﻠﻰ ﻤﻥ ﺍﻟﻘﺎﻨﻭﻥ ﺍﻟﺘﺎﻟﻲ-: RMR= 9 * Ln Q+26 ﻭ ﻟﻬـﺫﺍ ﻴﻤﻜـﻥ ﺤﺴﺎﺏ ﻗﻴﻤﺔ ﺘﺼﻨﻴﻑ ﺍﻟﻜﺘل ﺍﻟﺼﺨﺭﻴﺔ ﺒﺈﺤﺩﻯ ﺍﻟﻁﺭﻴﻘﺘﻴﻥ ﻭ ﻤﻥ ﺜﻡ ﺍﻴﺠﺎﺩ ﻗﻴﻤﺔ ﺍﻟﺘﺼﻨﻴﻑ ﺍﻷﺨﺭ ﻤﻥ ﺍﻟﻘﻭﺍﻨﻴﻥ ﺍﻟﺴﺎﺒﻘﺔ. د /ﻋﺒﺎس ﺑﻦ ﻋﻴﻔﺎن اﻟﺤﺎرﺛﻲ – ﻗﺴﻢ اﻟﺠﻴﻮﻟﻮﺟﻴﺎ اﻟﻬﻨﺪﺳﻴﺔ و اﻟﺒﻴﺌﻴﺔ -ﻛﻠﻴﺔ ﻋﻠﻮم اﻷرض -ﺟﺎﻣﻌﺔ اﻟﻤﻠﻚ ﻋﺒﺪ اﻟﻌﺰﻳﺰ. ﺻﻔﺤﺔ ٩ﻣﻦ .9 ﻣﻘﺮر ﻣﻴﻜﺎﻧﻴﻜﺎ اﻟﺼﺨﻮر
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