文章摘要
李娜,丁斌,顾泽凯,巩亮.不同复合页岩模型内气体竞争吸附特性的分子模拟[J].,2021,20(4):380-385
不同复合页岩模型内气体竞争吸附特性的分子模拟
Molecular simulation on competitive adsorption characteristics of gases in various composite shale models
投稿时间:2020-02-13  修订日期:2020-09-16
DOI:10.13738/j.issn.1671-8097.020024
中文关键词: 页岩气  吸附特性  蒙特卡洛方法  分子动力学
英文关键词: shale gas  adsorption characteristics  Monte Carlo  molecules dynamics
基金项目:国家自然科学基金(No. 51936001)及中央高校基本科研业务费专项资金(No.18CX07012A和No.19CX05002A)
作者单位E-mail
李娜 中国石油大学华东新能源学院 lina3727@126.com 
丁斌 中国石油大学华东新能源学院  
顾泽凯 中国石油大学(华东)新能源学院  
巩亮* 中国石油大学华东新能源学院 lgong@upc.edu.cn 
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中文摘要:
      构建了高岭石-干酪根IID、蒙脱石-干酪根IID和方解石-干酪根IID三种复合模型,采用巨正则蒙特卡罗方法(GCMC)和分子动力学方法(MD),从分子层面研究了CH4与注采气体(CO2、N2)在复合页岩材料中的吸附情况,分析了不同模型对不同气体的吸附能力。结果表明:在高岭石-干酪根IID复合模型中三种气体的吸附量为:NCO2>NCH4>NN2,其中CO2和CH4主要吸附于有机质微孔中,N2主要吸附于片层狭缝中。通过对比三种复合模型的吸附特性等温吸附曲线可以发现:蒙脱石-干酪根IID复合模型对CO2的吸附量最大,方解石-干酪根IID复合模型对CH4和N2的吸附量最大。此外,通过比较无机质与有机质对气体的吸附能力,发现有机质是页岩吸附能力的决定性因素。
英文摘要:
      To better guide the recovery of shale gas, three composite shale models ((kaolinite-kerogen IID, montmorillonite-kerogen IID and calcite-kerogen IID) are constructed in this paper. The giant regular Monte Carlo method (GCMC) and Molecules Dynamics method (MD) are adopted to explore the competitive adsorption characteristics between CH4 and injection gases (CO2, N2) in various composite shale models. The results show that the adsorption capacity of kaolinite-kerogen IID composite model for CO2, CH4 and N2 decreases gradually. Specifically, CO2 and CH4 are mainly adsorbed in organic micropores, by contrast N2 is mainly adsorbed in the interstitial slits. Moreover, the composite shale models present significant effects on the competitive adsorption characteristics. For instance, montmorillonite-kerogen IID composite model has the highest adsorption capacity for CO2, whereas, the calcite-kerogen IID composite model shows the highest adsorption capacity for CH4 and N2. Besides, by analyzing the adsorption capacity of inorganic matter and organic matter for gases, we find that the adsorption capacity of shale is governed by the organic matter.
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