摘要
同位素于地下水中的演变规律在水文地质领域的应用越来越广泛。通过沙漠区采用的水质同位素化验资料,作δD-δ18O关系图和矿化度-δ18O关系图,分析探讨沙漠区地下水的补给、运移、蒸发机理。
Isotope method is getting widely used to study goundwater movement in hydrogeology. On the basis of analysises of water quality isotope data,this paper discussed detailly the mechanism in desert with δD δ 18 O curve and SOD δ 18 O curve. The basic data are provided for groundwater exploitation for oil field water supply in desert zone.
出处
《世界地质》
CAS
CSCD
1997年第2期61-65,共5页
World Geology
关键词
同位素法
地下水
运移机理
沙漠区
油田
isotope method, δD,δ 18 O, groundwater movement in hydrogeology