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Analysis of seismic signatures from gas- and dust-based explosions at the Lake Lynn Experimental Mine

机译:林恩湖实验矿井瓦斯和粉尘爆炸的地震特征分析

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Examination of seismic records during the time interval of the Sago Mine disaster in 2006 revealed a small amplitude signal possibly associated with an event in the mine. More needs to be understood about the seismicity from mine explosions to properly interpret critical seismic information. A seismic monitoring system located at NIOSH's Lake Lynn Experimental Mine has monitored experimental gas-and dust-based explosions and impact tests. The seismic signatures from these different events were analyzed using standard waveform analysis procedures. The magnitude of seismic energy during a gas and dust explosion was found to be more dependent on mine entry geometry and seal behavior rather than on the amount of explosive fuel present. The results suggest a large explosion that is not restricted can generate potentially the same magnitude as a small explosion that is restricted.
机译:对2006年Sago矿山灾难期间的地震记录进行的检查显示,一个小振幅信号可能与矿山中的事件有关。为了正确解释关键的地震信息,需要更多地了解矿井爆炸的地震活动性。位于NIOSH的Lynn湖实验矿场的地震监测系统已经监测了基于气体和粉尘的爆炸和冲击试验。使用标准波形分析程序分析了这些不同事件的地震特征。发现在瓦斯和粉尘爆炸期间的地震能量的大小更多地取决于矿井入口的几何形状和密封行为,而不是取决于存在的爆炸性燃料的量。结果表明,不受限制的大爆炸可能会产生与受到限制的小爆炸相同的震级。

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