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

• Published in: Environmental geochemistry and health 2022-03, Vol.44 (3), p.961-977
• Main Authors: Gao, Zongjun, Han, Cong, Yuan, Shuyu, Liu, Jiutan, Peng, Yuming, Li, Changsuo
• Format: Article
• Language: English
• Subjects: Adult; Alluvial plains; Calcite; Calcium; Catchment area; Child; China; Cluster analysis; Contamination; Dolomite; Dolostone; Drinking water; Earth and Environmental Science; Entropy; Environment; Environmental Chemistry; Environmental Health; Environmental Monitoring; Evaporation; Geochemistry; Geology; Groundwater; Groundwater - analysis; Groundwater quality; Gypsum; Health risk assessment; Health risks; Humans; Hydrochemistry; Hydrogeology; Lake catchments; Lakes; Minerals; Nitrates; Original Paper; Pollution; Public Health; Soil Science & Conservation; Spatial analysis; Spatial distribution; Statistical analysis; Statistical methods; Sulphates; Terrestrial Pollution; Water analysis; Water Pollutants, Chemical - analysis; Water Quality; Water sampling
• ISSN: 0269-4042; 1573-2983
• DOI: 10.1007/s10653-021-01011-z

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–SO 4 ·Cl and Ca·Mg–HCO 3 , respectively, and that of Group III is more concentrated, mostly corresponding to the Ca–HCO 3 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.