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Quality Evaluation and its Controlling Factors of Groundwater from Wolonghu Mining Area, Northern Anhui Province, China

机译:皖北卧龙湖矿区地下水水质评价及其控制因素

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Major ion concentrations were analysed for 29 groundwater samples collected from diverse aquifersin Wolonghu mining, northern Anhui province, China. The evaluation of groundwater quality andcontrolling factors analysis were obtained by the methods such as multivariate statistical approachand conventional graphical and calculation of a series of index. The results showed that the groundwatersamples are alkaline in nature, with the high value of TDS ranging from 686 to 3927 mg/L, theconcentrations of Cl- are low for all groundwater samples, whereas the contents of SO42- and HCO3-are high. The groundwater samples of QA and CA could be used for drinking and irrigation, whereasthe groundwater of LA could not be used for irrigation for the high TDS concentration. The groundwaterin the area is mainly controlled by silicate weathering, the evaporative dissolution and carbonatedissolution. Sulphate dissolution also played an important role in the groundwater quality.
机译:分析了安徽省北部卧龙湖矿区不同含水层收集的29个地下水样品的主要离子浓度。通过多元统计方法,常规图形化和一系列指标计算等方法获得了地下水水质评价和控制因素分析结果。结果表明,地下水样品本质上是碱性的,TDS的高值在686-3927 mg / L之间,所有地下水样品的Cl-含量均较低,而SO42-和HCO3-的含量较高。 QA和CA的地下水样品可用于饮用水和灌溉,而LA的地下水不能用于高TDS浓度的灌溉。该地区的地下水主要受硅酸盐风化,蒸发溶解和碳酸盐溶解的控制。硫酸盐溶解在地下水质量中也起着重要作用。

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