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Overburden Migration and Failure Characteristics in Mining Shallow Buried Coal Seam with Thick Loose Layer

机译:采矿浅埋煤层厚覆盖煤层覆盖层的迁移和故障特性

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Quite a number of shallow buried coal seams (SBCS) are distributed in China. The overburden is easily damaged due to the mining of SBCS, resulting in water resources loss and surface damage. Taking 12403 working face of Wulanmulun coal mine in Shendong mining area as an example, this paper analyzed the overburden migration and failure characteristics after mining SBCS with thick loose layer based on actual measurement data and simulation results. The results show that the subsidence of strata in caving zone has no skewness feature along strike direction, while the subsidence of strata in fracture zone and bending subsidence zone shows skewness subsidence phenomenon. An interface exists in the overburden, and the movements of upper and lower strata at the interface have different characteristics. The cracks penetrating the whole strata exist in bedrock, not in aeolian sand. The height of water flowing fracture zone is 35.74?m–62.89?m according to the loss of fluid in the borehole and consistent with the results of numerical simulation and similar simulation. This study can provide a reference for the prediction of the height of water flowing fracture zone and the overburden migration in mining SBCS.
机译:相当多的浅埋煤层(SBC)在中国分发。由于SBC的采矿,覆盖层很容易损坏,导致水资源损失和表面损坏。在Shendong采矿区武兰梅森煤矿的12403个工作面,作为一个例子,分析了在基于实际测量数据和仿真结果的较厚宽松层的矿床迁移和失效特性。结果表明,洞区中层沉降沿着触发方向没有偏斜特征,而骨折区和弯曲沉降区中地层的沉降则表示偏斜沉降现象。覆盖层中存在一个接口,界面处的上层和下层的运动具有不同的特性。穿透整个阶层的裂缝存在于基岩中,而不是在风中。根据钻孔中的流体损失,水流动裂缝区的高度为35.74m-62.89Ωm。与数值模拟的结果和类似的模拟结果一致。该研究可以为预测水流动裂缝区的高度以及采矿SBCS中的覆盖层迁移的预测来提供参考。

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