准格尔矿区酸刺沟煤矿水文地球化学特征研究

    Research on Hydro-geochemical Characteristics in Suancigou Coal Mine of Zhungeer Coal Field

    • 摘要: 为了准确判别酸刺沟煤矿井下各出水点的充水水源,开展了不同含水层水文地球化学特征研究,结果表明:黄河侵蚀下切奥陶寒武地层,黄河东岸以泉的形式排泄补给黄河水,形成SO4·HCO3-Na·Ca型或Cl·SO4-Na·Mg型水;煤层顶底板各层水的水化学特征比较接近,均属于HCO3-Ca·Mg·Na型水;岩溶地下水通过黄河底部侧向补给黄河西部隐伏奥灰含水层,形成HCO3·Cl-Ca·Na型水,且奥灰水与黄河水有较密切的水力联系。分层聚类分析取距离阈值3,可以将所有水样分为4大类群,区分出各含水层水。

       

      Abstract: In order to discriminate water filling source of underground effluent points in Suancigou Coal Mine accurately, some technical means were used to research hydro-geochemical characteristics of each aquifer. The results show that karst water supplies Yellow River water due to Yellow River erodes Ordovician and Cambrian. The water chemical types are SO4·HCO3-Na·Ca and Cl·SO4-Na·Mg. The water chemical characteristic of coal seam roof and floor of each layer is close, and the water chemical type is HCO3-Ca·Mg·Na. Karst groundwater supplies concealed Ordovician aquifer in Yellow River west through the bottom of Yellow River, and forming HCO3·Cl-Ca·Na water, and there is close hydraulic relation between Ordovician water and Yellow River water. Hierarchical cluster analysis could divide all water samples into four major groups to distinguish water of each aquifer by taking distance threshold 3.

       

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