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Numerical simulation on mining effect influenced by a normal fault and its induced effect on rock burst

机译:正断层影响采动效应及其对岩爆影响的数值模拟

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The study of the mining effect influenced by a normal fault has great significance concerning the prediction and prevention of fault rock burst. According to the occurrence condition of a normal fault, the stress evolution of the working face and fault plane, the movement characteristics of overlying strata, and the law of fault slipping when the working face advances from footwall to hanging wall are studied utilizing UDEC numerical simulation. Then the inducing-mechanism of fault rock burst is revealed. Results show that in pre-mining, the in situ stress distribution of two fault walls in the fault-affected zone is notably different. When the working face mines in the footwall, the abutment stress distributes in a "double peak" pattern. The ratio of shear stress to normal stress and the fault slipping have the obvious spatial and temporal characteristics because they vary gradually from the higher layer to the lower one orderly. The variation of roof subsidence is in S-shape which includes slow deformation, violent slipping, deformation induced by the hanging wall strata rotation, and movement stability. The simulation results are verified via several engineering cases of fault rock burst. Moreover, it can provide a reference for prevention and control of rock burst in a fault-affected zone under similar conditions.
机译:研究正断层影响的开采效果对断层岩爆的预测和防治具有重要意义。根据正常断层的发生条件,利用UDEC数值模拟研究了工作面和断层面的应力演化,上覆地层的运动特征以及工作面从下盘壁向悬壁前进时的断层滑动规律。 。然后揭示了断层岩爆的诱发机理。结果表明,在采前,断层影响区的两个断层壁的原地应力分布明显不同。当工作面在下壁开采时,基台应力以“双峰”模式分布。剪应力与正应力之比和断层滑动具有明显的时空特征,因为它们从上层到下层逐渐变化。屋顶沉降的变化呈S形,包括缓慢的变形,剧烈的滑移,悬挂墙地层旋转引起的变形以及运动的稳定性。通过断层岩爆的几种工程实例验证了仿真结果。而且,它可以为类似条件下断层影响区的岩爆防治提供参考。

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