华北科技学院学报
華北科技學院學報
화북과기학원학보
JOURNAL OF NORTH CHINA INSTITUTE OF SCIENCE AND TECHNOLOGY
2013年
4期
1-5
,共5页
WY煤层气储层%深成变质作用%岩浆变质作用%吸附热%解吸率
WY煤層氣儲層%深成變質作用%巖漿變質作用%吸附熱%解吸率
WY매층기저층%심성변질작용%암장변질작용%흡부열%해흡솔
WY CBM reservoir%Plutonic metamorphism%Magmatic metamorphic effect%Heat of adsorption%Desorption rate
通过对深成变质作用与岩浆变质作用WY煤层气储层物质构成、孔隙发育、比表面积、吸附/解吸实验分析认为，WY变质类型的判定标志之一是小孔以下孔隙比例为96％。解吸作用方式取决于解吸热与吸附热的差值，晋城寺河地区井筒降压满足于WY煤层气解吸的能耗，解吸率高达66％。排水-降压-解吸的排采模式适应于本地区煤层气的开发。煤层气开采应以解吸热与吸附热差值为基础确定解吸方式。
通過對深成變質作用與巖漿變質作用WY煤層氣儲層物質構成、孔隙髮育、比錶麵積、吸附/解吸實驗分析認為，WY變質類型的判定標誌之一是小孔以下孔隙比例為96％。解吸作用方式取決于解吸熱與吸附熱的差值，晉城寺河地區井筒降壓滿足于WY煤層氣解吸的能耗，解吸率高達66％。排水-降壓-解吸的排採模式適應于本地區煤層氣的開髮。煤層氣開採應以解吸熱與吸附熱差值為基礎確定解吸方式。
통과대심성변질작용여암장변질작용WY매층기저층물질구성、공극발육、비표면적、흡부/해흡실험분석인위，WY변질류형적판정표지지일시소공이하공극비례위96％。해흡작용방식취결우해흡열여흡부열적차치，진성사하지구정통강압만족우WY매층기해흡적능모，해흡솔고체66％。배수-강압-해흡적배채모식괄응우본지구매층기적개발。매층기개채응이해흡열여흡부열차치위기출학정해흡방식。
By plutonic metamorphism and magmatic metamorphism WY CBM reservoir material composition , porosity develop-ment, surface area, adsorption /desorption experiments , Analysis, one of the hallmarks of WY metamorphic type to determine is the proportion of pores in the holes above 96%.Desorption mode of action depends on the difference between the heat of desorp-tion and heat of adsorption.Jin Cheng Si He wellbore antihypertensive to meet WY CBM desorption energy consumption , desorp-tion rate as high as 66%.Drainage-Step down -desorption mining model to adapt to the development of CBM in the region , CBM mining should be based on the difference between the heat of desorption and heat of adsorption and to determine the desorp -tion mode.
