热-力耦合作用下煤岩体渗流特性研究

    Study on coal permeability characteristics under thermo-mechanical coupling

    • 摘要: 煤层开采深度增加导致地温和应力增大,影响了煤样裂隙发育和渗流特性。为了研究热-力耦合作用下煤岩渗透过程中形变及渗透性变化特征,采用MTS815测试系统测试了50、100 ℃下6组煤样的全应力-应变过程中的渗透性。结果表明:温度为50 ℃时煤样抗压强度随围压增加而增加,4 MPa围压作用下煤样峰值偏应力达3.6 MPa,煤样轴向、环向应变均达到2%以上,表现出较高的延展性;温度为100 ℃时煤样抵抗变形能力下降,随围压增加,其峰值偏应力增加至4.9 MPa,煤样应变增长的速率加快;围压4 MPa、温度100 ℃时,煤样峰值渗透率达到3.5×10-11 m2;煤样加载过程中原始和新生裂隙扩展,孔隙连通性增强形成复杂的裂隙网络,热力效应使煤样渗流裂隙体积增加,渗透率增加。

       

      Abstract: The increase of coal mining depth leads to the increase of ground temperature and stress, which affects the development of fractures and seepage characteristics. In order to study the variation characteristics of deformation and permeability of coal under thermo-mechanical coupling, the MTS815 test system was used to test the permeability of six groups of coal samples during the whole stress-strain process at 50 ℃ and 100 ℃. The results indicated that: when the temperature set to 50 ℃, the compressive strength of coal samples increased with the increase of confining pressure. The peak deviator stress of the coal sample reached to 3.6 MPa under the confining pressure of 4 MPa, and the axial and circumferential strains both reached more than 2%, showing high performance of malleability. The deformation resistance of coal samples decreased when the temperature set to 100 ℃; with the increase of confining pressure, the peak deviant stress increased to 4.9 MPa, and the rate of strain growth accelerated. When the test condition set to 4 MPa and 100 ℃, the peak permeability of coal sample reached to 3.5×10-11 m2. The original and new fractures expanded, and the pore connectivity was enhanced to form a complex fracture network during the loading process. Then, the volume of seepage fractures and permeability of coal samples was increased by thermal effect.

       

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