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Role of water in the stability of a shallow, underground mine

机译:水在浅层地下矿山的稳定性中的作用

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A small underground mine in northern Idaho was used as an experimental facility for studying the role of water in the analysis of mine-opening stability. Laboratory test data, borehole measurements and geological mapping assisted in the construction of a coupled finite element model of the rock mass. The model was used to make quantitative estimates of rock stress, strain and displacement changes and to make estimates of the water pressure and flow velocity changes that occurred during historical mining. Stope cuts and wet fills were included in the analysis. The stability of the crown pillars between stopes was of particular interest. The relatively low effective stress and high rock-mass strength showed that water pressure changes were of no great consequence, which is in agreement with experience. The computational tools used in the analysis may be applied to other wet mines with appropriate changes to site-specific data.
机译:爱达荷州北部的一个小型地下矿井被用作实验设施,用于研究水在分析矿井稳定性方面的作用。实验室测试数据,井眼测量和地质测绘有助于构造岩体的耦合有限元模型。该模型用于定量估算岩石应力,应变和位移变化,并估算历史采矿过程中发生的水压和流速变化。分析中包括采场切割和湿填充。采掘场之间的冠状支柱的稳定性特别受关注。相对较低的有效应力和较高的岩体强度表明,水压的变化没有太大的影响,这与经验相吻合。分析中使用的计算工具可以应用于特定地点数据的适当更改的其他湿矿。

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