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Unraveling the hydrogeochemical characteristics and pollution sources of groundwater in an intensive industrial area, East China.
Huang, Xujuan; Ou, Li; Xie, Zhendong; Jiang, Chi; Zhao, Yibin; Wang, Guangcai.
Afiliación
  • Huang X; State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing, China.
  • Ou L; School of Water Resources and Environment, China University of Geosciences, Beijing, China.
  • Xie Z; Jiangxi Nonferrous Geological Mineral Exploration and Development Institute, Nanchang, China.
  • Jiang C; Jiangxi Province Ecological Environmental Monitoring Centre, Nanchang, China.
  • Zhao Y; Jiangxi Nonferrous Geological Mineral Exploration and Development Institute, Nanchang, China.
  • Wang G; Jiangxi Province Ecological Environmental Monitoring Centre, Nanchang, China.
Environ Sci Pollut Res Int ; 31(38): 50179-50197, 2024 Aug.
Article en En | MEDLINE | ID: mdl-39088176
ABSTRACT
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.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Contaminantes Químicos del Agua / Agua Subterránea / Monitoreo del Ambiente País/Región como asunto: Asia Idioma: En Revista: Environ Sci Pollut Res Int Asunto de la revista: SAUDE AMBIENTAL / TOXICOLOGIA Año: 2024 Tipo del documento: Article País de afiliación: China

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Contaminantes Químicos del Agua / Agua Subterránea / Monitoreo del Ambiente País/Región como asunto: Asia Idioma: En Revista: Environ Sci Pollut Res Int Asunto de la revista: SAUDE AMBIENTAL / TOXICOLOGIA Año: 2024 Tipo del documento: Article País de afiliación: China
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