原文服务方: 地球化学学报(英文)       
摘要:
Hydrogeochemistry and factor analysis were conducted together to assess the distribution and the major geochemical processes in fluoride-contaminated shallow groundwater in the Yuncheng Basin. Spatially, fluoride concentration was low (<1.5 mg/L) in the southern piedmont plain, medium (< 4 mg/L) in the central basin, and high (up to 14.1 mg/L) in Kaolao lowland areas in shallow aquifers. A three-factor principal component analysis model explained over 75.1% of the total variance. Sediment weathering leaching and evapotranspiration were recognized as the first primary hydrochemical processes response for the groundwater chemistry and explained the largest portion (42.1%) of the total variance. Factor two reflects the negative influence of human activities, with a positive loading of NO3- and HCO3-, and negative loading of well depth. Fluoride-bearing mineral dissolution and alkaline condition was ranked as the third factors responding for groundwater chemistry and explained 11.2% of the total variance.
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篇名 Distribution and assessment of hydrogeochemical processes of F-rich groundwater using PCA model: a c
来源期刊 地球化学学报(英文) 学科
关键词 Fluoride Groundwater chemistry PCA model Hydrogeochemical processes Yuncheng Basin
年,卷(期) 2022,(2) 所属期刊栏目
研究方向 页码范围 216-225
页数 9页 分类号
字数 语种 英文
DOI 10.1007/s11631-019-00374-6
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Fluoride
Groundwater chemistry
PCA model
Hydrogeochemical processes
Yuncheng Basin
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地球化学学报(英文)
双月刊
2096-0956
52-1161/P
大16开
贵州省贵阳市观水路46号地球化学研究所
1982-01-03
英文
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