4.6 Article

Assessment of the hydrochemistry, water quality, and human health risk of groundwater in the northwest of Nansi Lake Catchment, north China

Journal

ENVIRONMENTAL GEOCHEMISTRY AND HEALTH
Volume 44, Issue 3, Pages 961-977

Publisher

SPRINGER
DOI: 10.1007/s10653-021-01011-z

Keywords

Groundwater; Hydrochemistry; Water quality; Human health risk; The northwest of Nansi Lake Catchment

Funding

  1. National Natural Science Foundation of China [41772257, 41472216]
  2. Research Project of Shandong Province Bureau of Geology and Mineral Resources [KY2018003, KY201933]
  3. Shandong Provincial Geological Environment Exploration Project (2016) [3]
  4. China Postdoctoral Science Foundation [2020M682207]

Ask authors/readers for more resources

This study analyzed the formation mechanism and water quality of groundwater in the northwest of Nansi Lake Catchment through mathematical statistics, hydrochemical analysis, and entropy weighted water quality index (EWQI), and evaluated the human health risk of nitrate. The results showed that groundwater hydrochemistry is mainly influenced by water-rock interactions, with different groundwater quality among the three groups and overall good water quality, with low human health risk of nitrate.
In this study, the formation mechanism and water quality of groundwater in the northwest of Nansi Lake Catchment (NNLC) were analyzed through mathematical statistics, hydrochemical analysis and entropy weighted water quality index (EWQI), and the human health risk of nitrate was also evaluated. To this end, 89 wells in the NNLC were sampled, and the groundwater samples were divided into three groups (I, II, and III) according to cluster analysis results and spatial distribution. The main results are as follows: Topographically, Groups I, II, and III correspond to the alluvial plains, apron plain, and low hills and its front margin, respectively. According to the Piper diagram, the hydrochemical types of Groups I and II groundwater are Na-SO4 center dot Cl and Ca center dot Mg-HCO3, respectively, and that of Group III is more concentrated, mostly corresponding to the Ca-HCO3 type. Hydrochemical analysis indicated that the development of groundwater hydrochemistry is mainly attributable to water-rock interactions, with the primary process being the dissolution of minerals such as calcite, dolomite, gypsum, and albite. Evaporation exhibited an increasing trend from the northeast to the southwest. Groups I and III presented obvious effects of human activities, with Group I showing sulfate pollution and Group III mainly showing nitrate pollution. Analysis of the characteristics and causes of the groundwater hydrochemistry revealed the proposed approach has excellent performance for classification in areas with complex hydrogeological conditions. The results of EWQI showed that the overall water quality was good, following the order Group III > Group II > Group I. The overall human health risk of nitrate in groundwater was low, but the risk was slightly higher for children than for adults. Therefore, the effects of nitrate contamination should be considered when exploiting hilly and peri-urban groundwater for drinking water.

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