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Article

Factors Controlling Natural Background Levels of Ammonium and Iodide in Shallow Groundwater of Coastal Aquifers, South China

1
Haikou Marine Geological Survey Center, China Geological Survey, Haikou 570100, China
2
Zhejiang Dibo Survey and Design Co., Ltd., Hangzhou 310000, China
3
Faculty of Engineering, China University of Geosciences, Wuhan 430000, China
4
Zhejiang Engineering Geophysical Survey and Design Institute Co., Ltd., Hangzhou 310005, China
*
Author to whom correspondence should be addressed.
Water 2022, 14(22), 3737; https://doi.org/10.3390/w14223737
Submission received: 30 September 2022 / Revised: 18 October 2022 / Accepted: 28 October 2022 / Published: 17 November 2022
(This article belongs to the Special Issue Groundwater Chemistry and Quality in Coastal Aquifers)

Abstract

Assessing natural background levels (NBLs) in groundwater is crucial for evaluating groundwater pollution and the use of groundwater resources in coastal areas. This study assessed NBLs of iodide and ammonium in the shallow groundwater of the Pearl River Delta (PRD) by using a preselection method with Grubbs’ test, and discussed factors controlling NBLs in various groundwater units. Here, the preselection method consists of Cl/Br mass ratios versus Cl concentrations and the oxidation capacity, and the PRD is divided into four groundwater units. Results showed that NBL-iodide in groundwater unit A was 0.14 mg/L and >2 times greater than that in other groundwater units. Similarly, NBL-ammonium in groundwater unit A was 0.32 mg/L and also >2 times greater than that in other groundwater units. The release of iodide from both of organic-iodine in the vadose zone and iodine-rich minerals in aquifer sediments were the two main sources for the higher NBL-iodide in groundwater unit A compared to other units. By contrast, the occurrence of ammonium from organic-nitrogen in the vadose zone was the major source for the higher NBL-ammonium in groundwater unit A compared with the other units. Soluble iodide resulted from the mineralization of organic-iodine in Quaternary marine formation, and the release of iodide accompanied with reductive dissolution of iodide-loaded Fe (oxyhydr) oxides in aquifer sediments was the main driving force controlling the higher NBL-iodide in groundwater unit A compared with the other units. By contrast, the release of soluble ammonium from the mineralization of organic-nitrogen in marine formation entering into groundwater was the main driving force controlling the higher NBL-ammonium in groundwater unit A relative to the other units. These results enhance the knowledge on groundwater NBLs in coastal areas and improve groundwater resources management in coastal areas such as the PRD.
Keywords: natural background levels; iodide; ammonium; shallow groundwater; coastal areas natural background levels; iodide; ammonium; shallow groundwater; coastal areas

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MDPI and ACS Style

Pei, L.; Lu, X.; Li, X.; Zhang, M.; Wu, H. Factors Controlling Natural Background Levels of Ammonium and Iodide in Shallow Groundwater of Coastal Aquifers, South China. Water 2022, 14, 3737. https://doi.org/10.3390/w14223737

AMA Style

Pei L, Lu X, Li X, Zhang M, Wu H. Factors Controlling Natural Background Levels of Ammonium and Iodide in Shallow Groundwater of Coastal Aquifers, South China. Water. 2022; 14(22):3737. https://doi.org/10.3390/w14223737

Chicago/Turabian Style

Pei, Lixin, Xin Lu, Xiwen Li, Ming Zhang, and Heqiu Wu. 2022. "Factors Controlling Natural Background Levels of Ammonium and Iodide in Shallow Groundwater of Coastal Aquifers, South China" Water 14, no. 22: 3737. https://doi.org/10.3390/w14223737

APA Style

Pei, L., Lu, X., Li, X., Zhang, M., & Wu, H. (2022). Factors Controlling Natural Background Levels of Ammonium and Iodide in Shallow Groundwater of Coastal Aquifers, South China. Water, 14(22), 3737. https://doi.org/10.3390/w14223737

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