Li Jiawei, Wang Yuzhu, Chen Zhixi, Rahman Sheikh S
School of Minerals and Energy Resources Engineering, University of New South Wales, Sydney 2052, Australia.
Division of Physical Sciences and Engineering (PSE), King Abdullah University of Science and Technology (KAUST), Thuwal 23955-6900, Saudi Arabia.
Langmuir. 2021 Nov 2;37(43):12732-12745. doi: 10.1021/acs.langmuir.1c02274. Epub 2021 Oct 20.
Carbon dioxide (CO) injection in shale and coal seam gas reservoirs has become one of the most popular ways to promote methane (CH) production. However, geological factors affecting the CO enhanced gas recovery (CO-EGR) projects have not been studied in great depth, including underground moisture, subsurface water salinity, and other gases accompanying CH. Thus, a hybrid methodology of molecular dynamics (MD) and grand canonical Monte Carlo (GCMC) simulation is employed to reveal the gas adsorption and displacement mechanisms at a fundamental molecular level. This study generates a type II-D kerogen matrix as the adsorbent. The simulation environment includes 0-5 wt % moisture content, 0-6 mol/L NaCl saline, and 0-5 wt % CH for up to 30 MPa at 308, 338, and 368 K. The impressions of moisture, CH, and salinity on gas adsorption and competitive adsorption characteristics are analyzed and discussed. On the basis of the simulation results, the preloaded HO molecules negatively influence CH adsorption, leading to a 44.9% reduction at 5 wt % moisture content. Additionally, 6 mol/L NaCl within 5 wt % moisture content exhibits a further 9.8% reduction on the basis of the moisture effect. CH presents a more noticeable negative impact, of which 5 wt % results in a 73.2% reduction in CH adsorption. Moreover, the competitive process indicator, preferential selectivity , is analyzed and discussed in the presence of the mentioned factors. Moisture positively influences , salinity promotes , and CH develops . These factors would encourage the displacement processes of CH by CO injection. This study provides essential information for better gas resource estimation and gas recovery improvement in unconventional systems.
在页岩气和煤层气藏中注入二氧化碳(CO₂)已成为促进甲烷(CH₄)生产的最常用方法之一。然而,影响CO₂强化气藏开采(CO-EGR)项目的地质因素尚未得到深入研究,包括地下湿度、地下水盐度以及伴随CH₄的其他气体。因此,采用分子动力学(MD)和巨正则蒙特卡罗(GCMC)模拟的混合方法,从基本分子层面揭示气体吸附和驱替机制。本研究生成了II-D型干酪根基质作为吸附剂。模拟环境包括含水量0 - 5 wt%、NaCl盐水浓度0 - 6 mol/L以及CH₄含量0 - 5 wt%,在308、338和368 K温度下压力可达30 MPa。分析并讨论了湿度、CH₄和盐度对气体吸附和竞争吸附特性的影响。基于模拟结果,预先加载的H₂O分子对CH₄吸附产生负面影响,在含水量为5 wt%时导致CH₄吸附量降低44.9%。此外,在含水量为5 wt%的情况下,6 mol/L的NaCl在湿度影响的基础上使CH₄吸附量进一步降低9.8%。CH₄呈现出更显著的负面影响,其中5 wt%的CH₄导致CH₄吸附量降低73.2%。此外,在上述因素存在的情况下,对竞争过程指标——优先选择性进行了分析和讨论。湿度对优先选择性有积极影响,盐度促进优先选择性,而CH₄则使其增强。这些因素将促使通过注入CO₂来驱替CH₄。本研究为非常规系统中更好的天然气资源评估和提高气藏采收率提供了重要信息。