页岩纳米孔在静态和位移过程中对 CH4/CO2 的竞争吸附

IF 6.5 3区 工程技术 Q2 ENERGY & FUELS
Yulong Zhao , Mingyao Luo , Tao Zhang , Haoran Hu , Changcheng Yang , Qiang Luo , Bowen Guan
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引用次数: 0

摘要

在页岩气开发过程中,出现了单井产量低、衰退快、储层控制有限、采收率低等各种问题。提高页岩气储层采收率一直是业内的焦点和难题。因此,本文采用分子动力学(MD)模拟方法研究了不同温度和混合比下 CH4/CO2 的吸附和扩散特性。它比较了温度和 CH4/CO2 摩尔比变化对 CH4/CO2 的选择性系数、吸附容量和扩散系数的影响。论文还绘制了位移界面和 CH4/CO2 注入量/剩余量随时间变化的函数图。此外,论文还分析了分子在石墨烯表面的吸附能力、分子在狭缝中的迁移能力以及二氧化碳在纳米尺度上对 CH4 的置换过程,揭示了 CH4/CO2 竞争吸附和置换的微观机理。研究结果表明,温度对选择性系数的影响并不显著,温度每升高 20 K,选择性系数平均下降 3%。压力对选择性系数的影响更为明显,低压时的数值约为 1.4,高压时约为 1.2。提高二元气体混合物中 CO2 的摩尔分数会导致总吸附量的增加以及吸附量随压力的加速变化。随着 CH4 摩尔分数的增加,CH4 的扩散系数增大,而 CO2 的扩散系数则随着 CO2 摩尔分数的增加而减小。在相同条件下,CO2 在页岩有机纳米孔中的吸附能力强于 CH4,因此模型中出现了凹月形的位移界面。二氧化碳的预吸附压力越大,二氧化碳沿石墨烯表面的运动就越剧烈,二氧化碳沿孔壁的扩散速度就越快。在直径为 3 nm 的置换孔隙(用于提供置换位置或部位的孔隙空间)中,在较小的压差(≤10 MPa)下,CH4 的残留量保持相对稳定,不会发生实质性变化。然而,当压差达到 20 兆帕时,CH4 的残留量迅速减少,置换效率显著提高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Competitive adsorption of CH4/CO2 in shale nanopores during static and displacement process

During the development of shale gas, various issues such as low individual well production, rapid decline, limited reservoir control, and low recovery rates have arisen. Enhancing shale gas reservoir recovery rates has consistently been a focal point and challenge within the industry. Therefore, this paper employs molecular dynamic (MD) simulation methods to study the adsorption and diffusion characteristics of CH4/CO2 at different temperatures and mixing ratios. It compares the effects of temperature and CH4/CO2 molar ratio changes on the selectivity coefficient, adsorption capacity, and diffusion coefficient of CH4/CO2. The paper also plots the displacement interface and the function of CH4/CO2 injection/residual amounts over time. Furthermore, it analyzes the adsorption capacity of molecules on the graphene surface, the migration capacity of molecules in the slit, and the displacement process of CH4 by CO2 on the nanoscale, revealing the microscopic mechanism of CH4/CO2 competitive adsorption and displacement. The research results indicate that the influence of temperature on the selectivity coefficient is not significant, with an average decrease of 3% for every 20 K rise in temperature. Pressure has a more pronounced effect on the selectivity coefficient, with values around 1.4 at low pressures and around 1.2 at high pressures. Elevating the mole fraction of CO2 in the binary gas mixture results in an increase in the total adsorption amount and an accelerated variation of adsorption amount with pressure. As the CH4 mole fraction rises, the diffusion coefficient of CH4 increases, while the diffusion coefficient of CO2 diminishes with an increasing CO2 mole fraction. Under identical conditions, CO2 exhibits a stronger adsorption capacity over CH4 in shale organic nanopores, resulting in a concave moon-shaped displacement interface in the model. The larger the pre-adsorption pressure of CO2, the more intense the movement of CO2 along the graphene surface, and the faster the diffusion speed of CO2 along the wall. In a displacement pore (the pore space used to provide the displacement location or site) with a diameter of 3 nm, at smaller pressure differentials (≤10 MPa), the residual amount of CH4 remains relatively stable without substantial alteration. However, at a pressure differential of 20 MPa, the residual amount of CH4 decreases rapidly, and the displacement efficiency significantly improves.

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来源期刊
Natural Gas Industry B
Natural Gas Industry B Earth and Planetary Sciences-Geology
CiteScore
5.80
自引率
6.10%
发文量
46
审稿时长
79 days
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