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利用水化学和多元统计技术评估中国西北地区湟水河流域地下水化学的演化及其控制因素。

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.

机构信息

Hebei and China Geological Survey Key Laboratory of Groundwater Remediation, Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, China.

China University of Geosciences, Beijing 100083, China.

出版信息

Int J Environ Res Public Health. 2021 Jul 15;18(14):7551. doi: 10.3390/ijerph18147551.

Abstract

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, NO, SO, 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 HCO-Ca·Mg and HCO·SO-Ca·Mg. Additionally, high proportions of SO (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).

摘要

地下水是生态环境要素和人类生活及社会经济发展的关键性资源。了解地下水化学演化及其控制因素对于防止地下水恶化和确保地下水可持续利用至关重要。本研究采用水化学技术,研究了中国青海省湟水河流域地下水化学特征,并利用多元统计技术确定了该地区地下水化学的控制因素。2019 年 6 月,在 156 个采样点对地下水进行了 17 项水化学参数的调查。结果表明,总硬度、Fe、NO、SO 和 Cl 是该地区地下水的主要污染因子,分别有 33.3%、35.3%、8.97%、23.1%和 7.69%的样本超过中国地下水质量Ⅲ类标准。土地利用类型也显著影响地下水水化学。工业用地的地下水水化学组成受人类活动的影响更为强烈。该地区主要的地下水水化学类型为 HCO-Ca·Mg 和 HCO·SO-Ca·Mg。此外,SO(50.6%)、Na(32.1%)和 Cl(13.5%)等较高比例的地下水类型表明,人为活动对地下水水化学产生了影响。岩石风化是影响地下水水化学的主要因素,而蒸发浓缩和人为活动也影响了地下水的水化学特征。地下水的水化学组成主要受硅酸盐岩风化的控制。地下水水化学的主要控制因素为水岩相互作用、“物理化学”因素(自然过程)、生活污水、化肥和工业污水(人类活动)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/875c/8303299/77e7a2be6573/ijerph-18-07551-g001.jpg

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