水力耦合作用下煤变形及渗透率响应规律研究

    Study on deformation characteristics and permeability response of coal under hydro-mechanical coupling

    • 摘要: 煤层注水过程中,应力与水压产生耦合作用使煤体形变,影响煤岩渗流。为探究注水渗流过程中煤岩体积应变和渗透特性演化规律,利用岩石力学试验机,对煤岩开展水力耦合渗流试验,得出应力对煤岩渗透率和体积应变特征的影响规律,从而探究水压影响下煤岩体积应变和渗透特性演化规律。试验结果表明:渗透率对于体积应变存在着明显的响应规律,通过数据拟合得到煤岩渗透率和体积应变存在指数函数关系;恒定水压试验中,煤岩渗透率呈现先减后增的趋势,此过程试件经历了由压缩到扩展的过程,在煤岩裂隙贯通后渗透率达到极大值;变水压试验过程中,煤岩裂隙在较少的水压循环次数下处于压密状态,渗透率波动下降,但随循环次数增加,裂隙扩张,煤岩渗透率在水力耦合作用下开始增加;相同应力条件下,高孔隙水压促进裂隙扩展,促进体积应变量的增加以及渗透率的增长。

       

      Abstract: During the process of coal seam water injection, the coupling effect of stress and water pressure causes deformation of the coal, which affects the seepage. To explore the evolution law of the volume strain and permeability characteristics of coal during the seepage process of water injection, rock mechanics testing machine is used to carry out hydraulic coupling seepage test of coal. The influence law of stress on the permeability and volume strain characteristics of coal is obtained. On this basis, the evolution law of volumetric strain and permeability characteristics of coal under the influence of water pressure is studied. The experimental results show that there is a significant response law of permeability to volumetric strain, and the exponential function relationship between the permeability and volumetric strain of coal is obtained through data fitting. In the constant water pressure test, the permeability of coal shows a trend of decrease and then increase. During this process, the coal sample undergoes a transition from compression to expansion, and the permeability reaches its maximum value after the coal fractures are interconnected. During the alternating water pressure test, the coal fractures were observed to be compacted under lower water pressure cycles, leading to a decrease in permeability fluctuation. However, with the increase of the number of cycles and the expansion of fractures, the permeability of coal and rock begins to increase under the action of hydraulic coupling. Under the same stress condition, high pore water pressure promotes crack propagation, volume strain and permeability.

       

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