摘要
岳庄水源地地下水高氟的成因主要是地质、地貌和气候等因素。花岗片麻岩及其风化产物中含氟矿物的溶解是地下水中氟的主要来源。特殊的构造单元和较发育的断裂，是含氟水向地下运移的通道。水质类型、地貌。
The features of geology, geomorphlogy and climatology are the main causes of the high fluorine groudwater in water source area of Yuezhuang The fluorine in groundwater came form the dissolution of fluorine-bearing minerals in granite-gneiss and it′s weathering matter The special structure unit and developmental faults are passages in which fluorine-bearing water run to underground The type of water quality, landform and climate are the outside conditions that coused the high content of fluorine in groundwater
出处
《焦作工学院学报》
1997年第3期58-63,共6页
Journal of Jiaozuo Institute of Technology(Natural Science)
基金
煤炭部1996年年度基金
关键词
地下水
氟化物
含氟矿物
水源地
groundwater
fluoride
fluorine-bearing mineral
landform
climate
