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首页> 外文期刊>Environmental earth sciences >Three step-drawdown dewatering test in unsteady flow condition: a case study of the Siwan coal mine in North China Coalfield
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Three step-drawdown dewatering test in unsteady flow condition: a case study of the Siwan coal mine in North China Coalfield

机译:非恒定流条件下的三步降水脱水试验-以华北煤田四湾煤矿为例

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摘要

A dewatering test is a common tool to estimate the physical properties of water-bearing layers in coal mines. The three step-drawdown dewatering test of unsteady flow, which combines both steady and unsteady flows, is designed in this study. The test design involves the identification of hydrogeological conditions, calculation of hydrogeological parameters, and prediction of mine water yields, particularly those of the Siwan coal mine in the coal mining district of Hebi. The results show that the water storage and the abundance of the second limestone aquifer in Taiyuan formation (L-2) is limited and easy to drain, while the Ordovician system aquifer (O-2) lateral recharges the L-2 by the F-8 fault. The correlation curve method, the cone balance method, and the analytical method are conducted in this study. Results show that the average water yield was 1436.1 m(3)/h when the water level of L-2 decreased from + 127 m to + 17 m. The three step-drawdown dewatering test not only provides ways to enrich the experimental data and reveal hydrogeological conditions, but it can also be adopted in several approaches to predict mine water yields.
机译:脱水试验是评估煤矿含水层物理性质的常用工具。本研究设计了非稳态流的三步下降脱水试验,该试验结合了稳态流和非稳态流。测试设计涉及水文地质条件的识别,水文地质参数的计算以及矿井水产量的预测,特别是鹤壁煤矿区四湾煤矿的水产量。结果表明,太原组(L-2)第二石灰岩含水层的储水量和储量有限,易于排泄,而奥陶系含水层(O-2)通过F-向侧向补给L-2。 8故障。进行了相关曲线法,锥平衡法和分析法。结果表明,当L-2的水位从+ 127 m降至+ 17 m时,平均水产量为1436.1 m(3)/ h。三步降水脱水试验不仅提供了丰富实验数据和揭示水文地质条件的方法,而且还可以采用多种方法来预测矿井水的产量。

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