摘要
通过对大荔县地下水的采样调查,查明了高F水的分布、形成和富集规律。从气象、地质地貌、水文地质、水文地球化学等几个方面对高F水的成因进行了分析,结果显示,大荔县高F地下水的分布、形成和富集受地质地貌、水文地质和气候条件的控制,是以上各种因素长期综合作用的结果。在此基础上提出初步的治理措施,为解决大荔县饮水安全问题提供参考。
The distribution, formation and concentration characteristics of high-fluorine groundwater were made clear through sampling investigation of groundwater. The origin of high-fluorine groundwater was analyzed in the meteorological, geological, geomorphological, hydrogeological and hydrogeochemical contexts. The results show that the distribution, formation and concentration of high-fluorine groundwater were controlled by the geological, geomorphological, hydrogeological and climatic conditions and resulted from long-continued integrated effects of the aforesaid various factors. On that basis, the preliminary treatment measures were proposed as reference for solving the problem of safe drinking water in the Dali County.
出处
《地质通报》
CAS
CSCD
北大核心
2008年第8期1192-1195,共4页
Geological Bulletin of China
基金
中国地质调查局项目<陕西省大荔县高氟地下水调查评价>(编号:1212010634713)资助。
关键词
陕西大荔
高F水
分布特征
影响因素
Dali County, Shaanxi
high-fluorine groundwater
distribution
impact factor
