深井综采工作面过断层应力演化及岩层移动规律研究

    Study on stress evolution and strata movement law of deep well working face passing through fault

    • 摘要: 针对综采工作面过断层期间易发生片帮、冒顶等动力灾害,结合AB煤矿W1319工作面的煤层地质情况,采用理论分析、UDEC数值模拟并结合现场实测结果,综合研究垮落法管理顶板工作面过断层过程中覆岩的运动特征、采场煤岩体的破坏情况及应力分布规律。研究结果表明,处于应力平稳状态的工作面受到断层影响后采场应力异常增大,工作面推过断层后采场应力大幅减弱且断层两侧覆岩竖向位移有明显差异,说明断层对应力传播及塑性区的发育有明显阻隔作用,综采工作面过断层在经历了应力平稳阶段、应力异常增大阶段、应力递减阶段后,断层对工作面回采影响彻底消失,再次进入应力平稳阶段,数值模拟结果与现场实测结果一致。研究结果为综采工作面过断层期间安全高效生产提供了理论依据及技术指导。

       

      Abstract: In view of the dynamic disasters such as coal wall slabs and roof caving during the working face passing through the fault, combined with the coal seam geological conditions of the W1319 working face of Gaohe coal mine, using the theoretical analysis, UDEC numerical simulation combined with field measurement method, such as comprehensive research in the process of working face roof caving method management through the fault movement of overburden rock damage and the stress distribution characteristics.The results show that the stress in the steady state is affected by the fault, and the stress increases abnormally.After the working face pushes through the fault, the stope stress is greatly weakened and the vertical displacement of the overburden on both sides of the fault is obviously different.The propagation of the fault corresponding stress and the development of the plastic zone are obviously blocked.The fully mechanized mining face undergoes the stress stationary stage, the stress anomaly increases stage and the stress decreasing stage, and the fault has disappeared into the stress stationary stage again after the stress reduction stage.The results of numerical simulation are consistent with the result of field measurement.The research results provide theoretical basis and technical guidance for the safe and efficient production of fully mechanized mining face during fault crossing.

       

    /

    返回文章
    返回