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不同应力路径下含瓦斯裂隙煤岩组合结构损伤、渗流与能量协同演化

Synergistic evolution of damage, seepage and energy in gas-bearing fractured coal-rock composite structures under different stress paths

  • 摘要: 为厘清含瓦斯裂隙煤岩组合结构受载过程中损伤发展、渗流通道演化与能量储耗之间的内在联系,在初始围压4 MPa、瓦斯压力1 MPa条件下,设置完整试样及煤体、煤岩界面和岩体3类45°裂隙试样,并以界面裂隙试样为对象设置0°、30°、45°、60°和90°五种角度,分别开展常规三轴加载与同步加卸载试验,同步采集应力−应变、声发射和出口流量数据,并分析能量储耗特征。结果表明:裂隙位置与角度主要控制承载弱化程度、裂纹贯通路径及峰前储耗差异,应力路径主要改变损伤发展、增渗响应和能量转化的阶段分布。常规三轴加载下,界面裂隙试样峰值偏应力较完整试样降低51.8%;煤体裂隙、界面裂隙及小角度裂隙峰前损伤耗能较充分,岩体裂隙及大倾角裂隙则以弹性储能为主,损伤与增渗更趋向峰后。同步加卸载下,不同裂隙位置试样间的强度差异较常规三轴收窄,裂隙角度对峰后损伤集中程度的调节更加突出,45°、60°和90°试样峰后破坏阶段声发射计数占比达到95.3%~96.8%,高于0°和30°试样的67.1%~71.5%。与常规三轴相比,同步加卸载使完整及不同裂隙位置试样峰值偏应力降低12.2%~39.4%;不同角度试样峰后渗透率变化率提高187.1%~272.7%,峰值点总应变能密度和耗散能占比分别降低36.1%~68.9%和30.3%~71.1%。同步卸荷抑制平均应力增长并削弱裂隙闭合约束,压缩峰前稳定损伤与渐进耗能过程,使裂纹扩展贯通、声发射活动与增渗响应共同向峰值附近及峰后集中。损伤、渗流与能量响应分别表征裂纹活动、通道演化和能量转化,三者的协同变化受裂隙闭合、滑移、扩展和贯通过程共同控制。

     

    Abstract: To clarify the intrinsic relationships among damage development, seepage-channel evolution, and energy storage and dissipation in gas-bearing fractured coal-rock composite structures during loading, intact specimens and three types of specimens containing a 45° fracture located in the coal, at the coal-rock interface, or in the rock were prepared under an initial confining pressure of 4 MPa and a gas pressure of 1 MPa. Interface-fractured specimens with fracture angles of 0°, 30°, 45°, 60°, and 90° were also prepared. Conventional triaxial loading and synchronous loading-unloading tests were conducted for each configuration. Stress-strain, acoustic emission (AE), and outlet-flow data were recorded simultaneously, and the energy storage-dissipation characteristics were analyzed. The results show that fracture location and angle mainly control the degradation of load-bearing capacity, crack coalescence paths, and pre-peak energy storage-dissipation characteristics, whereas the stress path mainly alters the stage distribution of damage development, permeability enhancement, and energy conversion. Under conventional triaxial loading, the peak deviatoric stress of the interface-fractured specimen was 51.8% lower than that of the intact specimen. The coal-fractured, interface-fractured, 0°, and 30° specimens exhibited more pronounced pre-peak damage dissipation, whereas the rock-fractured, 60°, and 90° specimens were dominated by elastic energy storage, with damage and permeability enhancement tending to occur in the post-peak stage. Under synchronous loading-unloading, the differences in peak deviatoric stress among specimens with different fracture locations became smaller than those under conventional triaxial loading, while the fracture angle continued to exert a pronounced influence on the concentration of post-peak damage. The proportions of AE counts in the post-peak failure stage reached 95.3%−96.8% for the 45°, 60°, and 90° specimens, higher than the 67.1%−71.5% observed for the 0° and 30° specimens. Compared with conventional triaxial loading, synchronous loading-unloading reduced the peak deviatoric stress of the intact and differently located fractured specimens by 12.2%−39.4%, increased the post-peak permeability change rate of specimens with different fracture angles by 187.1%−272.7%, and decreased the total strain energy density and dissipated-energy ratio at peak stress by 36.1%−68.9% and 30.3%−71.1%, respectively. Synchronous unloading suppresses the increase in mean stress and weakens fracture-closure confinement, thereby compressing the stable pre-peak damage and progressive energy-dissipation processes and shifting crack propagation and coalescence, AE activity, and permeability enhancement toward the vicinity of the peak stress and the post-peak stage. Damage, seepage, and energy responses characterize crack activity, flow-channel evolution, and energy conversion, respectively, and their coupled evolution is jointly governed by fracture closure, slip, propagation, and coalescence.

     

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