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Using Coal Mine Water Inrush to Calculate Hydrogeological Parameters

机译:使用煤矿水涌计算水文地质参数

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In order to accurately analyze the reason of coal mine water inrush and study on coal mine hydrological condition, this paper takes coal mine water inrush as an aquifer dewatering test. Integrating hydrogeological drill, hydrogeological prospecting, hydrological monitoring system, etc. the paper provides an original groundwater seepage field recovery technique. And this technique was successfully applied to recover the original seepage field of the weathered Zhiluo Group roof aquifer of the 2~(-2) coal seam of the south panel of Ningtiaota coal mine. Based on the water inrush data collected by the hydrogeological monitoring system, this paper did an inverse calculation of the parameters of the aquifer. The permeability coefficients calculated from pumping test are 2.13m/d and 2.15m/d, while the coefficient from inverse calculation is 6.88m/d. The influence radiuses calculated from pumping test are 106m and 89m, while the influence radius from inverse calculation is 1941m. The results shows that the hydrogeological parameters calculated from water inrush inverse calculation are apparently bigger and more accurate compared to the parameters calculated from pumping test.
机译:为了准确分析煤矿涌入的原因和煤矿水文条件研究,本文将煤矿水浪涌作为含水层脱水试验。整合水文地质钻,水文地质勘探,水文监测系统等。本文提供了原始地下水渗流场恢复技术。这种技术成功地应用于恢复宁廷煤矿南部面板2〜(2)煤层的风化Zhiluo集团屋顶含水层的原始渗流场。根据水文地质监测系统收集的水涌入数据,本文对含水层的参数进行了反比计算。从泵送测试计算的渗透系数为2.13m / d和2.15m / d,同时从逆计算的系数为6.88m / d。从泵送测试计算的影响半径为106米和89m,而反向计算的影响半径为1941M。结果表明,与泵送试验计算的参数相比,从水中逆量计算计算的水文地质参数显然更大,更准确。

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