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Dynamic Analysis of the Rock Burst Potential of a Longwall Panel Intersecting with a Fault

机译:具有故障的长墙板与故障相交的岩石爆裂电位的动态分析

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Faults are one of the most common geological structures in underground mining. Affected by mining activities, fault-slip events will release large amounts of energy and trigger seismic waves, which could induce rock burst events and endanger mining operations. In this study, a longwall panel intersecting with a fault is introduced, as well as field microseismic (MS) monitoring. Static and dynamic numerical analyses are conducted to investigate the fault parameters' effects on the behaviors of the fault. The results show that the friction angle (phi(f)) significantly affects the shear displacement, magnitude and distribution of the seismic moment; the fault stiffness has a great effect on the magnitude of the seismic moment but smaller effects on the shear displacement and the distribution of the seismic moments. Based on the influence of the fault stiffness and phi(f) on the seismic moment, reasonable fault parameters can be determined. By employing the calibrated parameters, the dynamic responses and the rock burst potential of the surrounding rocks were analyzed by means of the peak particle velocity (PPV) and stress distribution. The propagation of the seismic waves released by fault-slip events excites the particle velocity of the rock mass, and there is a strong correlation between the particle velocity and rock mass damage. As the working face advances toward the fault, the PPV and stress fluctuation of the peak abutment stress rise significantly, which result in a great increase in the rock burst potential. The rock burst potential changes with the mining activities; therefore, corresponding measures must be applied to prevent and control rock burst events. This study contributes to deepening our understanding of the fault parameters in numerical simulations and the dynamic responses and rock burst potential of the surrounding rocks due to mining activities and provides a back-analysis calibration method for the fault parameters.
机译:故障是地下采矿中最常见的地质结构之一。受采矿活动的影响,故障净化事件将释放大量的能量和触发地震波,这可能会诱导岩爆事件和危险挖掘业务。在该研究中,引入了与故障交叉的长壁盘,以及现场微震(MS)监测。进行静态和动态数值分析,以研究故障参数对故障行为的影响。结果表明,摩擦角(PHI(F))显着影响地震时刻的剪切位移,幅度和分布;故障僵硬对地震时刻的大小具有很大的效果,对剪切位移的影响较小,以及地震时刻的分布。基于故障刚度和PHI(F)对地震时刻的影响,可以确定合理的故障参数。通过采用校准参数,通过峰值粒子速度(PPV)和应力分布来分析周围岩石的动态响应和岩石突发电位。故障流动事件释放的地震波的传播激发了岩体的粒子速度,颗粒速度和岩石质量损坏之间存在强的相关性。随着工作面向故障的进步,PPV和峰邻接应力的波动显着上升,这导致岩石突发潜力的大幅增加。岩石突破潜在的采矿活动变化;因此,必须应用相应的措施来防止和控制岩石突发事件。本研究有助于深化用户对数值模拟中的故障参数的理解以及由于采矿活动而导致周围岩石的动态响应和岩石爆裂电位,并为故障参数提供了反分析校准方法。

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