地质论评
地質論評
지질론평
GEOLOGICAL REVIEW
2015年
1期
207-216
,共10页
王茂桢%柳少波%任拥军%田华
王茂楨%柳少波%任擁軍%田華
왕무정%류소파%임옹군%전화
页岩气储层%粘土矿物%孔隙结构%比表面积%甲烷吸附
頁巖氣儲層%粘土礦物%孔隙結構%比錶麵積%甲烷吸附
혈암기저층%점토광물%공극결구%비표면적%갑완흡부
shale gas reservoir%clay mineral%pore structure%specific surface area%methane adsorption
粘土矿物是页岩的主要组成矿物,与页岩气的赋存和富集密切相关。粘土矿物因其特殊的晶体结构,在晶层之间、矿物内部以及矿物颗粒之间形成了不同类型的孔隙,这些孔隙的大小、形貌和比表面积决定着粘土矿物的甲烷吸附能力。为此,本文综述了粘土矿物的孔隙结构以及孔隙中的水和有机质对甲烷吸附性的影响,指出不同类型的粘土矿物孔隙发育与形貌特征存在差异,蒙脱石中多发育圆形、狭缝状的微孔且总比表面积最大,导致蒙脱石在所有粘土矿物中的甲烷吸附量最大;伊利石与高岭石中多发育中孔与大孔,吸附甲烷的能力低于蒙脱石。粘土矿物孔隙中的水与有机质显著影响到甲烷的吸附能力,水分子会占据孔隙表面,降低了甲烷的吸附能力,但可溶有机质对粘土矿物甲烷吸附能力的具体影响目前尚不明了。同时,根据页岩气勘探需求指出了本方向某些有待深入探讨的问题。
粘土礦物是頁巖的主要組成礦物,與頁巖氣的賦存和富集密切相關。粘土礦物因其特殊的晶體結構,在晶層之間、礦物內部以及礦物顆粒之間形成瞭不同類型的孔隙,這些孔隙的大小、形貌和比錶麵積決定著粘土礦物的甲烷吸附能力。為此,本文綜述瞭粘土礦物的孔隙結構以及孔隙中的水和有機質對甲烷吸附性的影響,指齣不同類型的粘土礦物孔隙髮育與形貌特徵存在差異,矇脫石中多髮育圓形、狹縫狀的微孔且總比錶麵積最大,導緻矇脫石在所有粘土礦物中的甲烷吸附量最大;伊利石與高嶺石中多髮育中孔與大孔,吸附甲烷的能力低于矇脫石。粘土礦物孔隙中的水與有機質顯著影響到甲烷的吸附能力,水分子會佔據孔隙錶麵,降低瞭甲烷的吸附能力,但可溶有機質對粘土礦物甲烷吸附能力的具體影響目前尚不明瞭。同時,根據頁巖氣勘探需求指齣瞭本方嚮某些有待深入探討的問題。
점토광물시혈암적주요조성광물,여혈암기적부존화부집밀절상관。점토광물인기특수적정체결구,재정층지간、광물내부이급광물과립지간형성료불동류형적공극,저사공극적대소、형모화비표면적결정착점토광물적갑완흡부능력。위차,본문종술료점토광물적공극결구이급공극중적수화유궤질대갑완흡부성적영향,지출불동류형적점토광물공극발육여형모특정존재차이,몽탈석중다발육원형、협봉상적미공차총비표면적최대,도치몽탈석재소유점토광물중적갑완흡부량최대;이리석여고령석중다발육중공여대공,흡부갑완적능력저우몽탈석。점토광물공극중적수여유궤질현저영향도갑완적흡부능력,수분자회점거공극표면,강저료갑완적흡부능력,단가용유궤질대점토광물갑완흡부능력적구체영향목전상불명료。동시,근거혈암기감탐수구지출료본방향모사유대심입탐토적문제。
The clay minerals are the main constituent minerals of the shale.It’s closely related with the occurrence and enrichment of shale gas.Because of its special crystal structure,clay minerals formed different types of pores between the crystal layers,in the internal mineral and between the mineral particles.The pore size, morphology and the specific surface area determine the methane adsorption capacity of the clay minerals.This paper reviews the occurrence of methane adsorption and various influence factors,such as pore structure,the water and organic matter in the pore.Different types of clay minerals are different in pore development and morphology.The round and slit micropores are most frequently found in smectite clay,which has the biggest total surface area and methane adsorption capacity.The mesoporous and macroporous are most developed in illite and kaolinite with the methane adsorption capacity belowing montmorillonite.Water and organic matters present in the pore of the clay minerals will also affect the methane adsorption capacity.Generally believed that water molecules will occupy the surface of pore,and resulting in a decrease of methane adsorption capacity of clay minerals.However,the specific effects of the soluble organic matter to the methane adsorption capacity of clay minerals are not clear yet.Finally, this paper indicates some of the issues to be explored in depth according to the needs of shale gas exploration.