Fluoride contamination, spatial variation, and health risk assessment of groundwater using GIS: a high-density survey sampling in Weifang City, North China

被引:0
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作者
Jiutan Liu
Yuanyuan Ma
Zongjun Gao
Yuqi Zhang
Zengbing Sun
Tianzhu Sun
Haibin Fan
Bin Wu
Mingbo Li
Lili Qian
机构
[1] Shandong University of Science and Technology,College of Energy and Mining Engineering
[2] Qingdao Geological and Mineral Geotechnical Engineering Co. Ltd,College of Earth Science and Engineering
[3] Shandong University of Science and Technology,undefined
[4] No 4 Exploration Institute of Geology and Mineral Resources,undefined
[5] Key Laboratory of Coastal Zone Geological Environment Protection,undefined
[6] Shandong Geology and Mineral Exploration and Development Bureau,undefined
[7] Tai’an Hydrological Center,undefined
关键词
Groundwater fluoride; Spatial variation; Health risk assessment; GIS; Weifang City;
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摘要
The present study, with the aid of GIS, utilizes high-density groundwater (GW) sampling data (1398 samples) to analyze the spatial variation characteristics of GW fluoride in Weifang City (WFC), and evaluate the health risks associated with drinking water routes. The concentration of fluoride in the GW of WFC is observed to be between 0.08 and 9.16 mg/L, with a mean value of 0.62 mg/L. The fluoride concentration of a total of 192 GW samples exceeded the limit of China’s GW quality standards (1 mg/L), accounting for 14.74%. The GW fluoride concentration in most areas of WFC is less than 1 mg/L. However, the relatively high-value zones are mostly concentrated in the upper reaches of Wen River, the east of Shouguang, the southeast of Anqiu, the east of Qingzhou, the east of Fangzi, and the southeast and northwest of Gaomi. The hydrochemical types of GW in WFC are mostly HCO3-Ca·Mg and SO4·Cl-Ca·Mg, while GW samples with hydrochemical types HCO3-Na and SO4·Cl-Na are characterized by high fluoride content. The hydrochemical characteristics of GW in WFC are mostly dominated by rock weathering. In addition, the northern coastal plain is evidently influenced by seawater intrusion. The concentration of fluoride in GW is affected by the dissolution of fluorine-containing minerals, cation exchange, and alkaline environmental factors. The effect of GW by seawater intrusion and very high content of Na+ will decrease the fluoride content of the GW through cation exchange. Health risk assessment demonstrated that the mean values of non-carcinogenic hazard quotient (HQ) for infants, children, teenagers, and adults were 0.52, 0.35, 0.31, and 0.30, respectively. In addition, the distribution characteristics of GW fluoride in high health risk areas (HQ > 1) in WFC are further consistent with the spatial variation of GW fluoride content. Overall, the health risk distribution area of GW fluoride in WFC is decreasing in the following order: infants > children > teenagers > adults.
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页码:34302 / 34313
页数:11
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