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Hydrogeochemical and water cycle features of groundwater at a western arid coal mine in the Ordos Jurassic coal province, China

机译:鄂尔多斯侏罗纪煤炭煤矿西部干旱地下水的水文和水循环特征

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Xiaojihan coal mine, located in the east of the Ordos basin, is typical of the regional hydrogeologic background and it commenced coal mining in 2014. To investigate water quality and water cycle features, 21 water samples were collected from underground aquifers for water quality tests, 14 samples for isotopes of D/~(18)O and T tests, and 6 samples for ~(14)C tests. The characteristics of the Jurassic aquifers are neutral pH, enriched in Na~+, high concentration of SO_4~(2-), large TDS, and polluted with B and E It was drawn that coal mining was inducing a much higher water connected zone than as expected and coal mining was dewatering and increasingly enlaring the depression cone in the Jurassic aquifers. It is urgent to limit the maxmum height of water interconnneted zone and control the further expansion of depression cone in the Jurassic aquifers.
机译:小济海煤矿位于鄂尔多斯盆地东部,是典型的区域水文地质背景,它于2014年开始煤炭开采。为了调查水质和水循环特征,从地下含水层收集21个水样的水质测试, 14个样品的D /〜(18)o和T检验同位素,6个样品〜(14)C试验。侏罗纪含水层的特征是中性pH,富含Na〜+,高浓度的SO_4〜(2-),大TDS,并用B和E污染,煤炭挖掘诱导比较高的水连接区随着预期的,煤炭开采脱水,越来越扩大了侏罗纪含水层的抑郁锥。迫切需要限制水互连区域的Maxmum高度,并控制侏罗纪含水层中抑郁锥的进一步扩张。

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