页岩有机质微纳米限域空间内甲烷吸附行为研究——以龙马溪组页岩为例OA
Methane adsorption behavior in confined space of shale kerogen:a case study of Longmaxi Formation shale
针对页岩微纳米限域空间内甲烷多元吸附行为难以厘定的问题,本研究对9组四川盆地龙马溪组页岩干酪根进行甲烷吸附实验,采用改进的Ono-Kondo模型分析了微纳米孔隙限域空间内的甲烷吸附行为.结果表明改进的Ono-Kondo模型更适用于页岩的甲烷吸附曲线表征.甲烷主要是以表面吸附和填充吸附的方式被吸附,并且填充吸附形式对甲烷总吸附能力贡献较大.甲烷的表面吸附行为主要发生在中孔中,其吸附能力随中孔体积增大而增大;而填充吸附行为主要发生在小于2 nm的微孔中,其吸附能力随微孔体积增大表现为对数型增大的规律.
To address the issue that methane multi-component adsorption behavior in shale micro-nano confined spaces is difficult to clarify,this study conducted methane adsorption experiment on 9 groups of shale kerogen samples from the Longmaxi Formation in the Sichuan Basin,and analyzed the meth-ane adsorption behavior in the confined spaces of micro-nano pores using an improved Ono-Kondo model.Results show that the improved Ono-Kondo model is more suitable for the characterization of methane adsorption behavior in shale kerogen.Methane is adsorbed in the nanopore by surface adsorp-tion and pore-filling adsorption,and the adsorbed methane in the form of pore-filling contributes sig-nificantly to the total methane adsorption amount.The surface adsorption behavior of methane mainly occurs in the mesopores,and its adsorption capacity increases with increasing mesopore volume.In contrast,the pore-filling adsorption mainly occurs in the micropores,and its adsorption capacity in-creases logarithmically with increasing micropore volume(<2 nm).
张楚;冯鹏;张雨恒
常州大学 安全科学与工程学院,江苏 常州 213164中国地质大学(北京)能源学院,北京 100083同济大学 土木工程学院,上海 200092
天文与地球科学
页岩气甲烷吸附分子模拟限域空间孔隙结构
shale gasmethane adsorptionmolecular simulationconfined spacepore structure
《常州大学学报(自然科学版)》 2026 (2)
57-64,8
国家自然科学基金资助项目(41872123)中国矿业大学煤层气资源与成藏过程教育部重点实验室开放研究基金资助项目(2023-006).
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