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鄂北岗地高氟地下水形成条件与改水降氟措施探讨
引用本文:郎文捷,周天慧. 鄂北岗地高氟地下水形成条件与改水降氟措施探讨[J]. 资源环境与工程, 2007, 21(4): 407-410
作者姓名:郎文捷  周天慧
作者单位:湖北省水文地质工程地质勘察院,湖北,荆州,434020;湖北省水文地质工程地质勘察院,湖北,荆州,434020
摘    要:鄂北岗地是湖北省有名的高氟地下水分布区,主要是浅层地下水中氟含量超标,它是在含氟矿物较多、孔隙潜水迳流不畅的高氟环境下形成的,因此,改水降氟应改饮含氟低的深井水。

关 键 词:鄂北岗地  高氟地下水  高氟环境  浅层地下水  改水降氟
文章编号:1671-1211(2007)04-0407-04
修稿时间:2007-02-07

Discussion of High-Fluorine Groundwater's Formation and Reducing the Content of Fluorine by Changing Water in Gangdi Area in the North of Hubei
LANG Wen-jie,ZHOU Tian-hui. Discussion of High-Fluorine Groundwater's Formation and Reducing the Content of Fluorine by Changing Water in Gangdi Area in the North of Hubei[J]. Resources Environment & Engineering, 2007, 21(4): 407-410
Authors:LANG Wen-jie  ZHOU Tian-hui
Abstract:Gangdi area is a famous distribution area of high-fluorine groundwater in the north of Hubei Province,and mainly content of F in the shallow groundwater exceeds the limited content.It is formed in high-fluorine condition of the mineral where fluorine is superscale and pore water unimpeded.Therefore,reducing the content of fluorine by changing the water means people should drink deep well water of low content of fluorine.
Keywords:Gangdi area in the north of Hubei  high F groundwater  high F condition  shallow groundwater  change water and reduce the content of F  
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