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Assessment of the Evolution of Groundwater Chemistry and Its Controlling Factors in the Huangshui River Basin of Northwestern China Using Hydrochemistry and Multivariate Statistical Techniques

机译:中国西北部黄水河流域地下水化学进化及其控制因素的评估采用水利化和多元统计技术

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摘要

Groundwater is an eco-environmental factor and critical resource required for human life and socioeconomic development. Understanding the evolution of groundwater chemistry and its controlling factors are imperative for preventing its deterioration and ensuring its sustainable use. We studied the characteristics of groundwater chemistry in the Huangshui River Basin in Qinghai Province, China using hydrochemical techniques. Additionally, we identified the controlling factors of groundwater chemistry in this region using multivariate statistical techniques. Seventeen hydrochemical parameters of groundwater were investigated at 156 sites in June 2019. The results showed that total hardness, Fe, NO3−, SO42−, and Cl− were primary pollution factors of groundwater in this region, and that 33.3%, 35.3%, 8.97%, 23.1%, and 7.69% of the samples exceeded Grade III standards for groundwater quality in China, respectively. Land use types also significantly affected groundwater hydrochemistry. The hydrochemical composition of groundwater in industrial areas is more strongly influenced by human activities. The major hydrochemical types identified in the region were HCO3-Ca·Mg and HCO3·SO4-Ca·Mg. Additionally, high proportions of SO4 (50.6%), Na (32.1%), and Cl (13.5%) groundwater types revealed the influence of anthropogenic activities on the groundwater hydrochemistry. Rock weathering was the major factor influencing the groundwater hydrochemistry, while evaporation–condensation and anthropogenic activities also influenced the hydrochemical characteristics of groundwater. The hydrochemical composition of groundwater was mainly controlled by silicate rock weathering. The main controlling factors of groundwater hydrochemistry were water–rock interactions, “physicochemical” factors (nature processes), domestic sewage, chemical fertilizer, and industrial sewage (human activities).
机译:地下水是一种生态环境因素和人类生活所需的批判资源和社会经济发展所需的资源。了解地下水化学的演变及其控制因素对防止其恶化和确保其可持续利用的迫切需要。我们研究了中国青海省黄水河流域地下水化学的特点,采用水利化学技术。另外,我们使用多元统计技术确定了该区域的地下水化学控制因素。在2019年6月在156个地点研究了17种水化学参数。结果表明,该地区地下水的总污染因子总,硬度,Fe,No3,So42-和Cl-是初级污染因素,33.3%,35.3%,35.3%,35.3%, 8.97%,23.1%和7.69%的样品分别超过中国的地下水质量等级标准。土地利用类型也显着影响地下水水化学。工业区地下水的水化工成分受到人类活动的强烈影响。该地区鉴定的主要水化学类型是HCO3-CA·Mg和HCO3·SO4-CA·MG。另外,SO4的高比例(50.6%),Na(32.1%)和Cl(13.5%)地下水类型揭示了人为对地下水氢化学的影响。岩石风化是影响地下水氢化学的主要因素,而蒸发 - 缩合和人为活性也影响了地下水的水化学特性。地下水的水化工学组成主要由硅酸盐岩石风化控制。地下水水化学的主要控制因素是水岩相互作用,“物理化学”因素(自然流程),国内污水,化肥和工业污水(人类活动)。

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