断层构造密集带采动围岩破坏规律研究

Study on the Failure Law of Mining-induced Surrounding Rock in Fault Structure Dense Zone

  • 摘要: 鲁西煤矿3128工作面(外段)中南部的断层密集带,在采动中易引发断层活化,加剧采空区围岩破坏,威胁煤炭生产安全。研究采用理论分析与FLAC3D数值模拟相结合的方法,构建围岩采动破坏模型,探究断层密集带对采动围岩破坏的影响规律,并与无断层密集带情况的理论计算结果对比。研究表明:断层密集带区域岩体完整性差、力学强度低,断层活化显著,围岩破坏程度严重;模拟得出导水裂隙带发育高度50 m、底板导水破坏带深度20 m,均高于无断层密集带时经验公式计算的37.17 m和11.31 m。该结论为复杂断层密集区域矿井安全生产提供科学参考。

     

    Abstract: The fault-intensive zone in the south-central part of the 3upper128 working face (outer section) of Luxi Coal Mine is prone to fault activation during mining, exacerbating the damage to surrounding rocks in the mined-out area and posing a threat to coal production safety. This study employs a combination of theoretical analysis and FLAC3D numerical simulation to construct a model of surrounding rock damage during mining, explore the influence of the fault-intensive zone on the damage to surrounding rocks during mining, and compare the results with theoretical calculations without the fault-intensive zone. The research indicates that the rock mass in the fault-intensive zone has poor integrity and low mechanical strength, with significant fault activation and severe damage to surrounding rocks. The simulation reveals a water-conducting fracture zone with a development height of 50 m and a water-conducting damage zone depth of 20m in the floor, both of which are higher than the values calculated by empirical formulas without the fault-intensive zone, which are 37.17 m and 11.31 m, respectively. This conclusion provides a scientific reference for safe production in mines located in complex fault-intensive areas.

     

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