胡青峰, 刘文锴, 崔希民, 李春意, 王新静. 煤柱群下重复开采覆岩与地表沉陷数值模拟实验[J]. 煤矿安全, 2019, 50(11): 43-47.
    引用本文: 胡青峰, 刘文锴, 崔希民, 李春意, 王新静. 煤柱群下重复开采覆岩与地表沉陷数值模拟实验[J]. 煤矿安全, 2019, 50(11): 43-47.
    HU Qingfeng, LIU Wenkai, CUI Ximin, LI Chunyi, WANG Xinjing. Numerical Simulation Experiment of Repeated Mining Overburden and Surface Subsidence Under Coal Pillar Group[J]. Safety in Coal Mines, 2019, 50(11): 43-47.
    Citation: HU Qingfeng, LIU Wenkai, CUI Ximin, LI Chunyi, WANG Xinjing. Numerical Simulation Experiment of Repeated Mining Overburden and Surface Subsidence Under Coal Pillar Group[J]. Safety in Coal Mines, 2019, 50(11): 43-47.

    煤柱群下重复开采覆岩与地表沉陷数值模拟实验

    Numerical Simulation Experiment of Repeated Mining Overburden and Surface Subsidence Under Coal Pillar Group

    • 摘要: 为研究煤柱群下重复开采覆岩与地表移动变形规律并揭示其形成机理,以某矿8104工作面地质采矿条件为工程背景,采用有限差分程序FLAC3D建立了其三维地质采矿模型,分别开展了2种情况下(采用刀柱式采煤方法仅开采上层煤和在煤柱群下进行重复开采)覆岩与地表沉陷数值模拟实验。结果表明:仅开采侏罗纪煤层时,覆岩与地表不会发生明显沉陷;在煤柱群下重复开采时,覆岩破坏形成“四带”发育特征,即由下往上依次为垮落带、断裂带、弯曲带和切冒带;研究区地表下沉系数小、下沉盆地范围较大以及地表沉陷容易形成非连续移动变形。

       

      Abstract: In order to study the overlying strata and surface subsidence laws due to repeated mining under coal pillar group and reveal its formation mechanism, this paper, taking the geological mining conditions of 8104 working face of a mine as the engineering background, established three-dimensional geological mining model by using finite difference program FLAC3D, and carried out numerical simulation experiments of overlying strata and surface subsidence under two conditions (mining only the upper coal with knife pillar method and mining repeatedly under coal pillar group ). The results show that only mining Jurassic coal, the overlying strata and surface subsidence is not obvious in the geological and mining conditions; repeated mining under the coal pillar group, the overlying strata destruction developed into “four zones”, namely from down to up in turn is caving zone, fracture zone, bending zone and caving zone; in the mine area, surface subsidence coefficient is smaller, subsidence basin range is larger and the surface subsidence is easy to form a non continuous movement and deformation.

       

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