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Numerical investigation of the use of hydraulic stimulation to mitigate fault slip risk in deep mines

机译:液压刺激利用液压刺激的数值调查,减轻深矿井故障滑动风险

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Fault slip and associated seismicity present a significant risk to the safety of underground mines. This paper investigates whether hydraulic stimulation, defined as the injection of pressurised fluid into a rock mass in advance of mining, has the potential to mitigate such risks. Fluid injected in the proximity of a critically-stressed pre-existing fault plane decreases the effective normal stress acting on the fault, initiating slip. Based on this concept, hydraulic stimulation could be used to trigger the release of built-up strain energy in advance of mining. Numerical investigations are carried out in a two-dimensional distinct element code to model the effect of injection on the slip of a pre-existing fault located adjacent to a conceptualised open stope mining operation. Injection is accompanied by slip and a significant decrease in shear stress acting on the fault. When no injection is performed, excavation triggers a series of slip events in response to the changing abutment stresses, generating a maximum M_w 1.3 event. Conversely, when hydraulic injection is performed prior to the mine excavation sequencing, the total number of slip events is reduced, and a lower maximum magnitude of M_w 1.1 is observed. Longer injection durations are observed to trigger larger areas of slip and greater total shear displacements. However, a consequence of injection activities is that stress becomes concentrated outside of the fluid propagation front, potentially triggering seismicity in areas where it was not originally anticipated.
机译:故障滑动和相关地震性对地下矿山的安全产生了重大风险。本文研究了液压刺激是否定义为在采矿前将加压流体注射到岩石肿块中,具有减轻这种风险的潜力。注入临床压力预先存在的断裂面附近的流体降低了作用于故障的有效正常应力,启动滑动。基于这一概念,可以使用液压刺激来引发挖掘之前释放内置应变能量的释放。在二维不同元件代码中进行数值研究,以模拟喷射对位于概念化的开放挖掘挖掘操作附近的预先存在的故障滑动的效果。注射伴随着滑动,并且在断层上作用的剪切应力显着降低。当未执行注入时,挖掘触发响应于变化的邻接应力,产生一系列滑动事件,产生最大M_W 1.3事件。相反,当在矿井挖掘测序之前进行液压喷射时,减小滑移事件的总数,并且观察到M_W 1.1的最大最大幅度。观察到较长的注射持续时间以触发更大的滑动区域和更大的总剪切位移。然而,注射活性的结果是,压力在流体繁殖前面的外部浓缩,潜在地触发原先预期的区域中的地震性。

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