工作面推进条件下承压水底板损伤破坏规律

Damage and failure laws of pressurized aquifer floor under conditions of working face advancement

  • 摘要:
    目的 为系统研究工作面带压开采条件下底板损伤破坏规律,
    方法 基于多孔介质、弹塑性力学与渗流力学理论,采用多场耦合数学物理控制方程,综合考虑应力、渗流压力的耦合作用,开展数值模拟分析。建立三维有限元模型,模拟不同推进距离(20~300 m)和含水层压力(1 MPa、2 MPa、3 MPa)下底板应力场与损伤演化特征。
    结果及结论 结果表明,工作面推进过程中底板水平应力持续累积,局部高应力区逐步扩展并在推进100 m后形成连续集中带。随着采动深入,底板损伤由浅部局部破坏演变为纵深贯通型破坏区,损伤系数最大可达0.9。水压对底板破坏具有显著促进作用,高承压条件下裂缝扩展范围和深度同步增强,破坏形态由分散性向“碗状”和“蝴蝶状”形态演化。在3 MPa的工况下,底板破坏带可穿透隔水层并与含水层连通,显著降低隔水性能,形成潜在导水通道。

     

    Abstract: To systematically study the damage and failure laws of the floor under the conditions of mining under pressure in the working face, based on the theories of porous media, elastoplastic mechanics and seepage mechanics, and using the multi-field coupling mathematical and physical control equations, a numerical simulation analysis was carried out, comprehensively considering the coupling effect of stress and seepage pressure. A three-dimensional finite element model was established to simulate the stress field and damage evolution characteristics of the floor under different advancing distances (20 m to 300 m) and aquifer pressures (1 MPa, 2 MPa and 3 MPa). The results show that during the advancement of the working face, the horizontal stress of the floor continuously accumulates, and the local high-stress area gradually expands and forms a continuous concentrated zone after advancing 100 m. With the deepening of mining, the floor damage evolves from local damage in the shallow part to a through-type damage zone in the depth, and the maximum damage coefficient can reach 0.9. Water pressure has a significant promoting effect on floor damage. Under high pressure conditions, the range and depth of crack propagation increase simultaneously, and the damage morphology evolves from a dispersed type to a "bowl-shaped" and "butterfly-shaped" type. Under the 3 MPa conditions, the floor damage zone can penetrate the aquiclude and connect with the aquifer, significantly reducing the water-blocking performance and forming a potential water-conducting channel.

     

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