Natural and anthropogenic factors regulating fluoride enrichment in groundwater of the Nansi Lake Basin, Northern China

Chunli Su; Mengzhu Wang; Xianjun Xie; Zhantao Han; Jiaqi Jiang; Zhen Wang; Dawei Xiao

doi:10.1016/j.scitotenv.2023.166699

Natural and anthropogenic factors regulating fluoride enrichment in groundwater of the Nansi Lake Basin, Northern China

Sci Total Environ. 2023 Dec 15:904:166699. doi: 10.1016/j.scitotenv.2023.166699. Epub 2023 Sep 1.

Authors

Chunli Su¹, Mengzhu Wang², Xianjun Xie², Zhantao Han³, Jiaqi Jiang², Zhen Wang⁴, Dawei Xiao⁴

Affiliations

¹ School of Environmental Studies, China University of Geosciences, Wuhan 430078, China; State Environmental Protection Key Laboratory of Source Apportionment and Control of Aquatic Pollution, Ministry of Ecology and Environment, Wuhan 430078, China. Electronic address: chl.su@cug.edu.cn.
² School of Environmental Studies, China University of Geosciences, Wuhan 430078, China; State Environmental Protection Key Laboratory of Source Apportionment and Control of Aquatic Pollution, Ministry of Ecology and Environment, Wuhan 430078, China.
³ Technical Centre for Soil, Agriculture and Rural Ecology and Environment, Ministry of Ecology and Environment, Beijing, 100012, China. Electronic address: hanzhantao@tcare-mee.cn.
⁴ Center for Soil Pollution Control of Shandong, Department of Ecological Environment of Shandong Province, Jinan 250101, China.

PMID: 37660817
DOI: 10.1016/j.scitotenv.2023.166699

Abstract

Excess fluoride (F^-) in groundwater can be hazardous to human health of local residents who rely upon it. Beside natural sources, anthropogenic input may be an additional source to be considered. Twenty surface water and 396 groundwater samples were collected from the Nansi Lake Basin, with hydrogeochemical and isotope techniques employed to clarify the spatial variability, source, and the natural and anthropogenic factors regulating the occurrence of high F^- groundwater. The factors responsible for elevated F^- levels in surface water and deep confined aquifers are discussed based on their hydraulic relationship. Also a conceptual model of F^- enrichment with different aquifer systems is put forward based on the geomorphic units of the basin. The results show that F^- concentration is between 0.1 and 6.9 mg/L in the west of Lake, while ranged from 0.03 to 1.74 mg/L in the east of Lake. The hydrogeological setting and lithology are the primary factor determining the provenance of high-fluoride groundwater in the basin. Fluoride mainly originated from the dissolution of fluorine-bearing minerals, and is affected by the alkaline groundwater environment, cation exchange, adsorption, and evaporation. The landforms on the east side of Nansi Lake are low hills and piedmont sedimentary plains, where the aquifers consist of karst fissure water and overlying porewater. High F^- groundwater is not observed in this area due to its rapid flow and Ca²⁺-enriched hydrochemical characteristics. The anthropogenic input (such as fertilizer application on farms and illegal industrial pollutant discharge), contribute F^- to groundwater in varying degrees, especially in the shallow aquifers east of the lake and in some parts west of the lake. This work is a clear example of how natural processes together with human activities can affect the chemical quality of groundwater, which is essential to safeguard the sustainable management of water resources in semi-arid areas.

Keywords: Conceptual model; Enrichment mechanism; Fluoride; Hydrochemical characteristics; Nansi Lake Basin.