应力水力耦合作用下底板岩体渗流突水规律

    Law of seepage and water inrush in floor rock mass under stress-hydraulic coupling

    • 摘要: 工作面开采扰动造成的底板损伤区是影响底板渗流突水的重要诱因,与底板岩层的脆性特征密切相关。为探究脆性底板与延性底板对地下含水层渗流突水的影响,采用RFPA数值模拟软件分析了2种岩性底板在应力扰动条件下的破坏特征与应力水力耦合条件下的渗流突水特征。结果表明:底板最大损伤深度随开采距离的增加呈现为正相关趋势。随着工作面的移动,底板最大损伤深度也会发生移动,底板延性越脆,底板损伤深度就越大。同时验证了脆性底板更容易诱发底板的渗流突水。揭示了煤层底板的脆性特性与工作面开采引起的底板损伤区深度之间的关系,为煤层底板渗流突水的危险评估和风险防控提供了参考。

       

      Abstract: The floor damage zone caused by mining disturbance in the working face is an important cause affecting the seepage and water inrush in the floor, which is closely related to the brittleness characteristics of the floor strata. In order to investigate the influence of brittle floor and ductile floor on seepage and water inrush of underground aquifer, the failure characteristics of two lithologic floor under stress disturbance and seepage and water inrush under stress hydraulic coupling were analyzed by RFPA numerical simulation software. The results show that the maximum damage depth of floor presents a positive correlation trend with the increase of mining distance. With the movement of the working surface, the maximum damage depth of the bottom plate will also move, and the more brittle the ductility of the bottom plate, the greater the damage depth of the bottom plate. At the same time, it is proved that brittle floor is more likely to induce seepage water inrush in the floor. The relationship between the brittleness characteristic of coal seam floor and the depth of damage zone of coal seam floor caused by mining is revealed, which provides a reference for the risk assessment and risk prevention of seepage water inrush in coal seam floor.

       

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