摘要
阐述了地下水中氟离子含量与氟本身的特性及地质、地貌、水文地质、人为因素的关系,分析了临汾市尧都区氟离子形成的原因,针对不同地区氟离子形成原因,提出了相应的解决方法:高氟区可采用集中供水方式;东部黄土台地区应采取打井或调水方式提供低氟水,最后提出治理含氟工业废水的方法。
This paper demonstrated the relationship between the concentration of fluorin ion in groundwater and related factors including the characteristics of fluoride, geology, physiography, hydrogeology, and human activities. In addition, how the fluoride came into being in groundwater was investigated. According to different fluoride origination processes observed in various areas, measures dealing with fluoride concentration in groundwater were proposed, for example, centralized water supply method should be adopted in regions with high concentration of fluorin ions; the water with low concentration of fluorin could be dug out from wells or transferred in loess platform regions in east Linfen. Finally the treatment methods for industrial wastewater with high concentration of fluorin were proposed.
出处
《水资源保护》
CAS
北大核心
2005年第5期76-78,共3页
Water Resources Protection
关键词
氟离子
地质
地貌
地下水
径流
临汾市
fluorin ion
geology and physiography
groundwater
runoff
Linfen City
