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Study on Permeability Anisotropy of Bedded Coal Under True Triaxial Stress and Its Application

机译:真三轴应力作用下层状煤渗透各向异性的研究与应用

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摘要

Anisotropy is a very typical observation in the intrinsic bedding structure of coal. To study the influence of anisotropy of coal structure and stress state on the evolution of permeability, a newly developed multifunctional true triaxial geophysical apparatus was used to carry out mechanical and seepage experiments on bedded coal. The permeability and deformation of three orthogonal directions in cubic coal samples were collected under true triaxial stress. It has detected the significant permeability anisotropy, and the anisotropy is firmly determined by the bedding direction and stress state of coal. Based on the true triaxial mechanical and seepage test results, the coal with bedding was simplified to be represented by a cubic model, and the dynamic anisotropic (D-A) permeability model was derived by considering the influence of bedding and stress state. The rationality of the permeability model was verified by the experimental data. Comparing the permeability model with Wang and Zang (W-Z) model, Cui and Bustin (C-B) model and Shi and Durucan (S-D) model, it is found that the theoretical calculated values of the D-A permeability model are in better agreement with the experimental measured values, reflecting the superiority of the D-A permeability model. Based on incorporating the model of D-A permeability under the concept of multiphysics field coupling, the numerical simulation experiments of coal seam gas extraction with different initial permeability anisotropic ratios were carried out by using COMSOL multiphysics simulator. The influence of initial permeability anisotropy ratio on gas pressure distribution in coal seam during gas extraction was explored, which provides theoretical guidance for the optimization of borehole layout for gas extraction in coal mine.
机译:各向异性是煤炭固有层理结构中非常典型的现象。为了研究煤结构各向异性和应力状态对渗透率演化的影响,采用了新型的多功能真三轴地球物理仪器对层状煤进行了力学和渗流实验。在真三轴应力下收集了立方煤样品中三个正交方向的渗透率和变形。它已经检测到明显的渗透率各向异性,并且各向异性是由煤层理方向和应力状态确定的。根据真实的三轴力学和渗流试验结果,简化了含顺层煤的立方模型,并考虑了顺层和应力状态的影响,得出了动态各向异性(D-A)渗透率模型。实验数据验证了渗透率模型的合理性。将渗透率模型与Wang和Zang(WZ)模型,Cui和Bustin(CB)模型以及Shi和Durucan(SD)模型进行比较,发现DA渗透率模型的理论计算值与实验测量值更好地吻合。值,反映了DA渗透率模型的优越性。基于多物理场耦合概念下的D-A渗透率模型,利用COMSOL多物理场模拟器对不同初始渗透率各向异性的煤层气进行了数值模拟实验。探讨了初始渗透率各向异性比对瓦斯抽采过程中煤层瓦斯压力分布的影响,为优化煤矿瓦斯抽采井眼布置提供了理论指导。

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