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Correlating seismic wave velocity measurements with mining activities at Williams Mine

机译:威廉姆斯矿井采矿活动的地震波速度测量

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Seismic wave velocities are sensitive to rock mass properties including fracture density, orientation, stress magnitude and orientation. By measuring small changes, of the order of 0.01%, in the seismic wave velocities over time, it is possible for track changes in the rock mass properties to occur. In mining, the rock mass properties are altering as the rock is removed or pillars are formed. By tracking these changes, it may be possible to get a better understanding of the effect mining has on the rock mass properties. These changing rock mass properties are important for reliable static stress modelling of the mine and for stability analysis. We use an active seismic source where a pneumatic hammer generates repeatable impacts that can be measured a few hundred metres away from the source. This allows us to measure directional velocity changes where these can be compared with mining and microseismic activity. This is the first step in understanding the effect of mining on the rock mass properties over time.
机译:地震波速度对岩体质量特性敏感,包括断裂密度,取向,应力幅度和取向。通过测量小变化,在随着时间的推移时,在地震波速度下,在地震波速度下,可以进行岩石质量特性的轨道变化。在采矿时,岩体质量特性随着岩石被移除或形成柱而改变。通过跟踪这些变化,可以更好地理解岩石质量特性的效果开采。这些变化的岩石质量特性对于矿井的可靠静态应力建模和稳定性分析非常重要。我们使用活跃的地震源,气动锤产生可重复的冲击,可以从源距离源几百米的距离。这使我们能够测量与挖掘和微震活动进行比较的定向速度变化。这是了解采矿对岩石质量特性的影响的第一步。

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