摘要
通过对运城盆地高氟地下水分布规律及成因探讨,确认高氟是由半干旱的气候条件、富含氟化物的包气带土体、碱性的地球化学环境及独特的水文地质构造确定,并详细地揭示了区内高氟地下水的形成机理。
Distribution and formation of high-fluorine groundwater in Yuncheng basin were discussed in this paper. It is presented that high-fluorine is caused by the semi-arid climate of the region, high-fluorine content of soils in the saturated zone, alkaline geo-chemical environment, and the unique hydrogeological structure. The formation mechanism of highfluorine groundwater in this region was also studied.
出处
《水资源保护》
CAS
北大核心
2005年第6期63-65,共3页
Water Resources Protection
关键词
地下水
运城盆地
氟含量
groundwater
Yuncheng basin
content of fluorine
