Unraveling the hydrogeochemical characteristics and pollution sources of groundwater in an intensive industrial area, East China

被引:0
|
作者
Huang, Xujuan [1 ,2 ,3 ]
Ou, Li [4 ]
Xie, Zhendong [3 ]
Jiang, Chi [4 ]
Zhao, Yibin [3 ]
Wang, Guangcai [1 ,2 ]
机构
[1] State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing, China
[2] School of Water Resources and Environment, China University of Geosciences, Beijing, China
[3] Jiangxi Nonferrous Geological Mineral Exploration and Development Institute, Nanchang, China
[4] Jiangxi Province Ecological Environmental Monitoring Centre, Nanchang, China
关键词
Self organizing maps;
D O I
10.1007/s11356-024-34511-3
中图分类号
学科分类号
摘要
It is challenging to interpret hydrogeochemical datasets with complex natural and anthropogenic genesis in intensive industrial areas. This paper elucidates the hydrogeochemical characteristics and pollution sources of groundwater in an industrial park, East China, combining the self-organizing map (SOM), hydrochemical graphs, and correlation analysis. The results show that the total dissolved solids of groundwater range from 73.45 to 997.92 mg/L and can be regarded as freshwater. The pH varies greatly from 6.44 to 9.90, most of samples belonging to weakly acidic-weakly alkaline. The groundwater can be classified into five clusters by SOM, representing the non- or least-polluted groundwater (cluster D), high salt groundwater (cluster A), high NH4+-N and HCO3− groundwater (cluster B), high Fe and Mn groundwater (cluster C), and high pH groundwater (cluster E), which were contaminated by industrial salts, historical agriculture activity, industrial reducing substances, and industrial alkali, respectively. The natural evolution of groundwater (cluster D) in the study area is mainly controlled by mineral weathering/dissolution. The contributions of calcite, dolomite, gypsum, halite, and silicate mineral to groundwater solute are 55.8–66.3%, 15.1–18.0%, 9.0–10.7%, 2.5–10.1%, and 2.3–9.4%, respectively, based on the mass conservation. The contaminated groundwaters (all other clusters except for cluster D) have different hydrochemical characteristics associated with the pollution sources. In addition, the relatively reductive environment in quaternary flu-lacustrine sediments favored the formation of high level of Fe, Mn, and NH4+-N in groundwater. This study provides a new insight into the characteristic contaminants and their distributions in groundwater and the associated pollution sources based on the large datasets in an intensive industrial area. The data evaluation methods and results of this study could be useful to the groundwater usage management and pollution control in this area and other industrial areas. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024.
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页码:50179 / 50197
页数:18
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