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Stability Analysis and Failure Evolution of Large-scale Underground Caverns in Layered Rock Masses from Microseismic Monitoring

机译:微震监测中分层岩体大规模地下洞穴的稳定性分析与故障演变

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To assess the stability of large-scale underground caverns excavated in a layered rock mass with layers dipping steeply inside the surrounding rock, a high-resolution microseismic monitoring system was carried out in the right underground powerhouse of the Wudongde hydropower station in Southwest China. The progressive processes of layered rock mass damage including the initiation, propagation, coalescence and interaction of rock micro-fractures, was first demonstrated by analyzing the temporal and spatial distribution of microseismic activities. Meanwhile, the microseismic monitoring results were validated using conventional monitoring data and field observations. A typical failure of layered rock masses was fortunately monitored and the evolution of the microseismicity and its corresponding mechanism during the development of this studied failure were also obtained. The results can provide us an overall understanding of the progressive damage and failure evolution of large-scale underground openings in bedded rock masses.
机译:为了评估在层状岩体中挖掘的大型地下洞穴的稳定性,在周围岩石内浸泡层,在中国西南部的沃隆德水电站的右下地下厂房进行了高分辨率微震监测系统。通过分析微震活性的时间和空间分布,首先首先通过分析微震活动的时间和空间分布,首先进行分层岩体质量损伤的逐步过程,包括岩石微骨折的开始,繁殖,聚结和相互作用。同时,使用常规监测数据和现场观察验证微震监测结果。还获得了分层岩体的典型故障,并且还获得了这种研究失败期间微震性和相应机制的进化。结果可以全面了解大型地下开口的逐步损坏和失效演变。

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