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Underground Mine Site Investigations for Estimating Hydrogeological Properties of Regional Fractured Rock Aquifers

机译:地下矿山现场估算区域骨折岩含水层水文地质性质的研究

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A number of analytical models developed either for mines, tunnels or for collector wells can be used to estimate the hydraulic conductivity of a regional aquifer in fractured rock based on data collected at underground mines, in spite of uncertainties affecting the data and the models. Hydraulic conductivity values obtained for the three mine sites (Beaufor, CANMET and Lac Herbin) are presented as intervals of possible values associated with each method. The most probable values are situated between 1.6 × 10~(-9) m/s and 4.6 × 10~(-9) m/s, the lowest estimate being 2.0 × 10~(-10) m/s and the highest 4.4 × 10~(-8) m/s.
机译:尽管有影响数据和模型的不确定性,但是,可以使用用于矿山,隧道或收集器井的矿山井的分析模型来估计裂缝岩中的区域含水层的液压导电性,尽管有影响数据和模型的不确定性。为三个矿位点(Beaufor,Canet和LAC草蛋白)获得的液压导电值作为与每种方法相关的可能值的间隔呈现。最可能的值位于1.6×10〜(-9)m / s和4.6×10〜(-9)m / s,最低估计为2.0×10〜(-10)m / s,最高4.4 ×10〜(-8)m / s。

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