断层影响下导水裂缝带发育高度研究

    Study on the development height of water conducting fracture zones under the influence of faults

    • 摘要: 导水裂缝带发育高度是水体下采煤最重要的参数之一,煤层开采易诱发断层活化,导致导水裂缝带发育高度增大。针对断层对导水裂缝带发育高度难以判断的问题,采用数值模拟研究了工作面开采覆岩塑性区分布、应力和位移变化情况,并与经验公式进行了对比,阐述了断层影响导水裂缝带发育高度增大的机制。研究结果表明:断层影响下工作面回采覆岩塑性区明显增大,断层附近应力集中,岩层下沉量增大;与无断层经验公式预计结果相比,无断层影响导水裂缝带发育高度为22.17~36.84 m,导水裂缝带发育高度为无断层发育高度1.2~2.1倍;采动影响下,断层切割破坏了岩层的整体性,影响采动应力的传播,在断层附近产生应力集中,导致断层活化,导水裂缝带发育增大。研究成果可为类似条件下水体下采煤提供理论基础与应用参考。

       

      Abstract: The development height of the water conducting fracture zone is one of the most important parameters for coal mining under water bodies. Coal seam mining can easily induce fault activation, leading to an increase in the development height of the water conducting fracture zone. In response to the difficulty in determining the height of water conducting fracture zones caused by faults, numerical simulations are used to study the distribution of plastic zones, stress, and displacement changes in overlying rock during mining. The results show that under the influence of faults, the plastic zone of the overlying rock in the mining face significantly increases, stress concentration near the fault increases, and the subsidence of the rock layer increases. Compared with the expected results of the empirical formula without faults, the development height of the water conducting fracture zone without faults is 22.17-36.84 m, and the development height of the water conducting fracture zone without faults is 1.2-2.1 times that of the development height without faults. Under the influence of mining, fault cutting destroys the integrity of rock layers, affects the propagation of mining stress, and causes stress concentration near the fault, leading to fault activation and the development of water conducting fracture zones. The research results can provide theoretical basis and application reference for coal mining under similar conditions in water bodies.

       

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