Source tracing analysis of the exceedance of NH3-N and CODMn in shallow groundwater in the central typical area of the Yangtze river delta

With the accelerated urbanization process in the Yangtze River Delta region, shallow groundwater has received increasing attention. In this work, the exceedances of the ammonium nitrogen (NH<sub>3</sub>-N) and chemical oxygen demand (COD<sub>Mn</sub>) in shallow groundwater in the central typical area of the Yangtze River Delta were investigated. With the utilization of the national monitoring well (QY10A) as a focal point, a combination of methods, including onsite sampling, hydrogeological surveys, leaching tests, water quality analysis, and isotope tracing, was employed to comprehensively examine groundwater pollution. The study addressed the history of groundwater exploitation, changes in surface water quality, and the influence of stratigraphic structure on groundwater contamination. It has been observed that the NH<sub>3</sub>-N levels in the silty chalky clay layer and the lower grayish black chalky clay layer in the study area are notably elevated, with concentrations reaching up to 87.5 mg/kg and 97.4 mg/kg in some boreholes. The NH<sub>3</sub>-N concentration in the silty clay with silty sand can reach as high as 87.2 mg/kg, whereas the concentration is lower in the underlying layers. In the other strata, NH<sub>3</sub>-N values remain low. The results indicated that the NH<sub>3</sub>-N and COD<sub>Mn</sub> in the QY10A monitoring well resulted primarily from the inherently high organic nitrogen content in the local geological environment rather than from anthropogenic sources such as industrial parks, domestic sewage, or agricultural activities. This finding highlights the critical role of geological conditions in influencing groundwater quality, emphasizing the necessity of considering these natural factors in pollution prevention and management strategies. Our research provides valuable insights for environmental management in similar geological settings and demonstrates the importance of scientifically rigorous methods for advancing environmental research and policy-making.

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Publication Details

Journal
Scientific Reports
Published
2024-11-18
DOI
https://doi.org/10.1038/s41598-024-79579-6
Citations
6
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
2.08

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article

Source tracing analysis of the exceedance of NH3-N and CODMn in shallow groundwater in the central typical area of the Yangtze river delta

zhongxia li, Kexin Li, Shuqin Li, Xiangmei Li et al.
6 citations
Scientific Reports
Groundwater and Isotope Geochemistry
2.08
article

Source tracing analysis of the exceedance of NH3-N and CODMn in shallow groundwater in the central typical area of the Yangtze river delta

zhongxia li, Kexin Li, Shuqin Li, Xiangmei Li, Li Wan, Wei Guo
article en
6 citations

Abstract

With the accelerated urbanization process in the Yangtze River Delta region, shallow groundwater has received increasing attention. In this work, the exceedances of the ammonium nitrogen (NH<sub>3</sub>-N) and chemical oxygen demand (COD<sub>Mn</sub>) in shallow groundwater in the central typical area of the Yangtze River Delta were investigated. With the utilization of the national monitoring well (QY10A) as a focal point, a combination of methods, including onsite sampling, hydrogeological surveys, leaching tests, water quality analysis, and isotope tracing, was employed to comprehensively examine groundwater pollution. The study addressed the history of groundwater exploitation, changes in surface water quality, and the influence of stratigraphic structure on groundwater contamination. It has been observed that the NH<sub>3</sub>-N levels in the silty chalky clay layer and the lower grayish black chalky clay layer in the study area are notably elevated, with concentrations reaching up to 87.5 mg/kg and 97.4 mg/kg in some boreholes. The NH<sub>3</sub>-N concentration in the silty clay with silty sand can reach as high as 87.2 mg/kg, whereas the concentration is lower in the underlying layers. In the other strata, NH<sub>3</sub>-N values remain low. The results indicated that the NH<sub>3</sub>-N and COD<sub>Mn</sub> in the QY10A monitoring well resulted primarily from the inherently high organic nitrogen content in the local geological environment rather than from anthropogenic sources such as industrial parks, domestic sewage, or agricultural activities. This finding highlights the critical role of geological conditions in influencing groundwater quality, emphasizing the necessity of considering these natural factors in pollution prevention and management strategies. Our research provides valuable insights for environmental management in similar geological settings and demonstrates the importance of scientifically rigorous methods for advancing environmental research and policy-making.

Scientific ReportsVol. 14(1)
Huawei Technologies (China) (CN), China University of Geosciences (Beijing) (CN), Yanshan University (CN), Sinosteel (China) (CN), China Nonferrous Metal Mining (China) (CN), Institute of Mining (RU), Masteel (China) (CN), Anhui University of Technology (CN)
National Key Research and Development Program of China
Life below water
Openalex Percentile: Top 14%
Groundwater and Isotope Geochemistry
2.08
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