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Influence of gas migration on permeability of soft coalbed methane reservoirs under true triaxial stress conditions

机译:真三轴应力条件下瓦斯运移对软煤层气储层渗透率的影响

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The permeability of the coal body is the key parameter restricting the efficient extraction of coalbed methane, and scholars have analysed it from two angles of the change of stress state and porosity of the coal body. However, there is still a lack of study on the mechanism of gas migration and movement in soft coalbed methane reservoir under the coupling between the true triaxial stress field (maximum principal stress σ 1 intermediate principal stress σ 2 minimum principal stress σ 3 ) and the gas pressure field. In this paper, the coal gas adsorption and seepage experiments are conducted through the self-developed true triaxial ‘gas–solid’ coupled coal mass seepage system with gas as the adsorption and seepage medium and coal briquette taking the place of soft coalbed methane reservoirs. Furthermore, the coal gas adsorption deformation model and the permeability evolution model taking gas adsorption into account are developed. Through analysis of both experimental and theoretic results, the main conclusions are drawn as follows: (i) With the increase in gas pressure, the adsorption deformation variation of coal mass is divided into a slow growth zone, a stable growth zone and a rapid growth zone. (ii) The gas adsorption deformation model developed can predict the variation trend of coal mass adsorption volumetric strains for different types of soft coalbeds, and the fitting variance of experimental and theoretical volumetric strains is above 98%. (iii) With the increase in maximum principal stress difference, the coal permeability variation curve shows two obvious turning points, which can be divided into a slow reduction zone, a rapid reduction zone and a steady reduction zone. (iv) The permeability model of coal mass considering the gas adsorption effect can reflect the variation characteristics of permeability in the rapid reduction zone, and the overall fitting variance of experimental and theoretical permeabilities is above 91%. The above results could provide a reliable experimental and theoretical basis for improving coalbed methane extraction rates.
机译:煤体的渗透率是制约煤层气有效开采的关键参数,学者从应力状态变化和煤体孔隙度两个角度对其进行了分析。但是,在真三轴应力场(最大主应力σ1>中间主应力σ2>最小主应力σ3)之间的耦合作用下,软煤层气储层瓦斯运移运动机理尚缺乏研究。和气压场。本文通过自行开发的真三轴“气固耦合”煤质渗流系统,以瓦斯为吸附和渗流介质,并以煤团块代替了软煤层气储层,进行了瓦斯吸附和渗流实验。建立了考虑气体吸附的煤气吸附变形模型和渗透率演化模型。通过对实验结果和理论结果的分析,得出以下主要结论:(i)随着气压的升高,煤质的吸附变形变化分为缓慢增长区,稳定增长区和快速增长区。区。 (ii)建立的瓦斯吸附变形模型可以预测不同类型软煤层的煤质吸附体积应变的变化趋势,实验体积应变和理论体积应变的拟合方差均在98%以上。 (iii)随着最大主应力差的增加,煤的渗透率变化曲线显示出两个明显的转折点,可分为缓慢还原区,快速还原区和稳定还原区。 (iv)考虑瓦斯吸附作用的煤体渗透率模型可以反映快速还原带渗透率的变化特征,实验渗透率和理论渗透率的整体拟合方差均在91%以上。以上结果可为提高煤层气抽采率提供可靠的实验和理论基础。

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