Long-term evolution mechanisms of permeability during gas injection for enhanced coalbed methane recovery

IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Lei Yang , Chaojun Fan , Mingkun Luo , Quanle Zou , Ce Jia , Qiwang Sun , Zhiheng Cheng
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Abstract

Understanding the long-term evolution of permeability during gas (N2 or CO2) injection for enhanced CBM recovery (G-ECBM) is of great significance for improving CBM recovery efficiency and achieving effective CO2 sequestration. This study develops a thermo-hydro-mechanical (THM) coupled model to comprehensively capture the mechanical response, fluid transport, and thermal variations during G-ECBM. The model is validated and subsequently employed to elucidate the long-term evolution mechanisms of permeability under N2 and CO2 injection from the standpoint of coal strain. N2-ECBM significantly improves CH4 recovery rate, but the rapid breakthrough of N2 reduces CH4 concentration. In contrast, the recovery rate of CO2-ECBM is lower than that of N2-ECBM, but it maintains a relatively high CH4 concentration consistently. At early stage of N2-ECBM, the permeability decreases near production well (PW) as effective stress increases, while the permeability increases near injection well (IW) as effective stress decreases. Later, coal seam permeability increases as effective stress decreases and CH4 desorption. For CO2-ECBM, early permeability near PW shows minimal change as effective stress increases offsets CH4 desorption, while later stages see reduces driven by CO2 adsorption. Near IW, early permeability increases due to CH4 desorption outweighs CO2 adsorption, but later declines as CO2 adsorption becomes stronger. The offer provides a basis for optimizing injection strategies and improving recovery rate.
煤层气提高采收率注气过程渗透率的长期演化机制
了解注气(N2或CO2)提高煤层气采收率(G-ECBM)过程中渗透率的长期变化规律,对于提高煤层气采收率和实现有效的CO2封存具有重要意义。本研究建立了一个热-水-机械(THM)耦合模型,以全面捕捉G-ECBM过程中的机械响应、流体输运和热变化。对模型进行了验证,并从煤应变的角度阐明了N2和CO2注入下渗透率的长期演化机制。N2- ecbm显著提高了CH4的回收率,但N2的快速突破降低了CH4的浓度。相比之下,CO2-ECBM的回收率低于N2-ECBM,但始终保持较高的CH4浓度。在N2-ECBM早期,随着有效应力的增加,生产井附近渗透率降低,而注入井附近渗透率随着有效应力的减小而增加。随后,煤层渗透率随着有效应力的减小和CH4的解吸而增大。对于CO2- ecbm, PW附近的早期渗透率变化最小,因为有效应力增加抵消了CH4的解吸,而后期渗透率则因CO2吸附而降低。在IW附近,由于CH4解吸作用大于CO2吸附作用,早期渗透率增加,但随着CO2吸附作用的增强,后期渗透率下降。这为优化注入策略和提高采收率提供了基础。
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来源期刊
CiteScore
14.00
自引率
5.60%
发文量
196
审稿时长
18 weeks
期刊介绍: The International Journal of Rock Mechanics and Mining Sciences focuses on original research, new developments, site measurements, and case studies within the fields of rock mechanics and rock engineering. Serving as an international platform, it showcases high-quality papers addressing rock mechanics and the application of its principles and techniques in mining and civil engineering projects situated on or within rock masses. These projects encompass a wide range, including slopes, open-pit mines, quarries, shafts, tunnels, caverns, underground mines, metro systems, dams, hydro-electric stations, geothermal energy, petroleum engineering, and radioactive waste disposal. The journal welcomes submissions on various topics, with particular interest in theoretical advancements, analytical and numerical methods, rock testing, site investigation, and case studies.
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