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王刚, 肖智勇, 王长盛, 蒋宇静, 于俊红. 基于非平衡状态的煤层中气体运移规律研究[J]. 岩土工程学报, 2022, 44(8): 1512-1520. DOI: 10.11779/CJGE202208016
引用本文: 王刚, 肖智勇, 王长盛, 蒋宇静, 于俊红. 基于非平衡状态的煤层中气体运移规律研究[J]. 岩土工程学报, 2022, 44(8): 1512-1520. DOI: 10.11779/CJGE202208016
WANG Gang, XIAO Zhi-yong, WANG Chang-sheng, JIANG Yu-jing, YU Jun-hong. Gas transport in coal seams based on non-equilibrium state[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(8): 1512-1520. DOI: 10.11779/CJGE202208016
Citation: WANG Gang, XIAO Zhi-yong, WANG Chang-sheng, JIANG Yu-jing, YU Jun-hong. Gas transport in coal seams based on non-equilibrium state[J]. Chinese Journal of Geotechnical Engineering, 2022, 44(8): 1512-1520. DOI: 10.11779/CJGE202208016

基于非平衡状态的煤层中气体运移规律研究

Gas transport in coal seams based on non-equilibrium state

  • 摘要: 煤层气开采过程中,由于裂隙与基质渗透率性能差异性较大,导致储层在长时间内都将处于非平衡的动态调整阶段。然而,目前大多数的试验和渗透率模型只考虑某一固定气体压力的影响,这极大地限制了对非平衡状态下储层气体流动的研究。为此,基于储层为双重孔隙介质的概念,考虑开采过程中基质–裂隙不同的孔隙压力、解吸变形和力学作用对裂隙开度演化的影响,提出了一种预测气体在非平衡状态下的渗透率模型,并用现场数据进行了验证。进一步将渗透率模型代入气体流动方程,采用有限元软件分析了岩芯内基质–裂隙的孔隙压力和渗透率随时空的演变规律。研究结果表明:在岩芯解吸过程中,①岩芯内裂隙气体压力受扰动范围大于基质气体压力;②基质–裂隙气体压力和渗透率沿岩芯长度呈现非线性分布;③基质–裂隙渗透率变化趋势相同。

     

    Abstract: During extraction of coalbed methane, the reservoir will be in a non-equilibrium dynamic adjustment phase for a long period of time due to the high variability of fracture and matrix permeability properties. However, most of the current tests and permeability models only consider the effects of a certain fixed gas pressure, which greatly limits the study of reservoir gas flow under non-equilibrium condition. Therefore, based on the concept that the reservoir is a dual porous medium, and considering the effects of different pore pressures, desorption deformation and mechanical effects of matrix-fracture on the evolution of fracture aperture during the extraction process, a model is proposed to predict the reservoir permeability under variable stress states and validated through the field data. Then the model is substituted into the gas flow equation, and the pore pressure of matrix–fracture and the evolution of core permeability in time and space are studied separately by using the finite element software. The results show that during the core desorption: (1) The fracture gas pressure in the core is disturbed to a greater extent than the matrix gas pressure. (2) The gas pressure and permeability of matrix–fracture exhibit non-linear distribution along the core length. (3) The permeability of matrix–fracture varies in the same trend.

     

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