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Molecular simulation of CO2/CH4 competitive adsorption in organic matter pores in shale under certain geological conditions

机译:在一定条件下页岩有机质孔隙中CO 2 / CH 4 竞争吸附的分子模拟地质条件

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摘要

To reveal competitive absorption behavior between CH4 and CO2 in organic matter (OM) nanopores, OM pore structure was first characterized using focused ion beam?scanning electron microscope (FIB-SEM) and pore-size distribution was studied using N2 adsorption, using Lower Silurian Longmaxi shale in Sichuan Basin as sample. Then a simplified pillar-layer model was used to study CH4 adsorption behavior and competitive adsorption effect between CO2 and CH4, using grand canonical Mote Carlo (GCMC) method. Research indicates that nanopores with good connectivity widely exist in OM, offering important storage space for absorbed shale gas. The amount of absorbed CH4 can increase with lower temperature and increased pressure, and overpressure will significantly increase the amount of CH4 absorbed underground; CO2 shows high competitive absorption ability; CO2/CH4 selectivity coefficient decreases dramatically with increasing temperature or pressure, or both, and it corresponds to deeper burial depth. CO2 EGR during shale gas exploration will be more efficient if it is conducted after the pressure drops to a certain degree.
机译:为了揭示有机物(OM)纳米孔中CH4和CO2之间的竞争吸收行为,首先使用聚焦离子束-扫描电子显微镜(FIB-SEM)表征了OM的孔结构,并使用N2吸附和下志留纪研究了孔径分布以四川盆地龙马溪组页岩为例。然后,采用简化的柱-层模型,采用大规范Mote Carlo(GCMC)方法研究CH4的吸附行为和CO2与CH4之间的竞争吸附效果。研究表明,OM中广泛存在具有良好连通性的纳米孔,为吸收的页岩气提供了重要的储存空间。较低的温度和较高的压力会增加吸收的CH4量,过压会显着增加地下吸收的CH4量。 CO2具有很高的竞争吸收能力; CO2 / CH4选择性系数随温度或压力(或两者)的增加而急剧下降,并且对应于更深的埋藏深度。如果在压力下降到一定程度后进行页岩气勘探过程中的CO2 EGR,效率将会更高。

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