4.3 Article

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

Publisher

MDPI
DOI: 10.3390/ijerph18147551

Keywords

groundwater; hydrochemical characteristics; controlling factors; human activities; multivariate statistical techniques

Funding

  1. projects of China Geological Survey, China [DD20190331]
  2. Fundamental Research Funds for the Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences [SK202117]
  3. China Postdoctoral Science Foundation [2020M670448]

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The study investigated the groundwater chemistry characteristics and controlling factors in the Huangshui River Basin in Qinghai Province, China. Major pollution factors identified were total hardness, Fe, NO3-, SO42-, and Cl-. The study also found that factors impacting groundwater chemistry included groundwater types, land use types, and human activities such as sewage and industrial discharges.
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 center dot Mg and HCO3 center dot SO4-Ca center dot 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).

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