永城矿区高氟地下水的氟源及其地质构造因素——永城矿区高氟污染地下水成因探讨之一  

The source of high fluorine content in groundwater and its geological structure factors in Yongcheng mining area

作　　者：尹国勋[1] 付新峰[1] 赵群华 张威[3] 

机构地区：[1]焦作工学院,河南焦作454000 [2]永城煤电公司城郊矿,河南永城476600 [3]河北工业大学,河北石家庄050000

出　　处：《焦作工学院学报》2002年第2期110-113,共4页Journal of Jiaozuo Institute of Technology(Natural Science)

基　　金：煤炭工业部 1996年攻关项目 (96 3 5 3 )"华北煤矿区高氟;高硫水的成因与处理"的一部分

摘　　要：研究了永城矿区高氟地下水中氟的来源及其地质构造控制因素 .认为地层中含氟矿物的溶解是深层地下水中氟的天然来源 ,而土壤中含氟矿物及土粒表面呈吸附态的氟是该区浅层地下水中氟的主要物质来源 .该区独特的地质构造为含氟水进入提供了通道 。In this paper,the authors have analysed the source of high fluorine content in groundwater and its structue factors in Yongcheng mining area.The authors have considered that dissolving the contain fluorine mineral is nature source of fluorine in the depths of groundwater and that fluorine?bearing minerals in soil and fluorine absorbed on surface of soil are primary source of fluorine in the shallow of groundwater.Geological structure has provided passageway for high florine content water to get into subterranean and constituted the unit within groundwater converged from all directions.

关 键 词：永城矿区 地下水 氟源 地质构造 含氟矿物 土壤 

分 类 号：P641.461[天文地球—地质矿产勘探] TD163.1[天文地球—地质学]