Hydrochemical Evolution Mechanisms of Shallow Groundwater and Its Quality Assessment in the Estuarine Coastal Zone: A Case Study of Qidong, China

Yao Wen, Jiahao Qiu, Si Cheng, Changchang Xu and Xiaojiang Gao
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Yao Wen: Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
Jiahao Qiu: Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
Si Cheng: Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
Changchang Xu: Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China
Xiaojiang Gao: Department of Environmental Science and Engineering, Fudan University, Shanghai 200433, China

IJERPH, 2020, vol. 17, issue 10, 1-23

Abstract: Identification of geochemical characters and the influence of river and seawater on coastal areas are of significant impact on water resources management in coastal areas globally. Thus, it requires careful investigation of the hydrochemical evolution mechanisms and assessment of the quality of shallow groundwater. The study specifically focused on the estuarine coastal zone of Qidong, China, a city located on the Yangtze estuary. Thirty shallow groundwater samples and five surface water samples were collected during a field investigation, and 25 water quality indexes were analyzed. Methods including mathematical statistics, Gibbs figure, Piper diagram, and ionic rations were used to analyze the hydrochemical characteristics and evolution mechanisms. The spatial distribution of key parameters was assessed using a GIS-based spatial gridding technique. Results showed that the shallow groundwater in this estuarine coastal zone is weakly alkaline. The major hydrochemical parameters, including total dissolved solids (TDS), Na + and Cl − , Mg 2+ , and SO 4 2− , displayed similar spatial distributions; the distributions of Ca 2+ and Mg 2+ were irregular; the distributions of SO 4 2− and HCO 3 − shared a similar trend, increasing gradually from the southern to northern regions of the study zone; and the values of NO 3 − and NH 4 + were generally low in the study area. The hydrochemistry of the groundwater consists of HCO 3 -CaMg type and HCO 3 -Na, with HCO 3 ·Cl-Na type and Cl-Na being the dominant constituents toward the coastal strip. The coastal aquifers are subjected to the ongoing influence of seawater intrusion, ion exchange processes, freshwater infiltration, and mineral (carbonate and silicate) dissolution, which impact groundwater evolution. Most of the groundwater samples are unsuitable for drinking purposes, but more than 90% of samples have irrigation suitability, based on the WHO standards and the classifications of sodium absorption ratio (SAR), soluble-sodium percentage (SSP).

Keywords: hydrochemistry; shallow groundwater; coastal zone; Yangtze estuary; groundwater quality (search for similar items in EconPapers)
JEL-codes: I I1 I3 Q Q5 (search for similar items in EconPapers)
Date: 2020
References: View complete reference list from CitEc
Citations: View citations in EconPapers (1)

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