摘要
本文讨论了河北平原地下咸水的同位素组成。并且依据水文地质、水化学和同位素特征将咸水成因分为两种类型,即大陆盐化成因和海水成因咸水。前者δ18O<-7.00‰,δD<-55.0‰,36Cl/Cl>57±9(×10-15),14C年龄为1000~4000a(校正);后者δ18O>-7.00‰,δD>-55.0‰,δ37Cl值接近海水值,14C年龄大于10000a(校正),咸水中的海水百分比大于38.0%。
This paper discusses the isotopic compositions of saline groundwater in Hebei plain and divides the saline water genetically into two types based on the hydrogeological,hydrochemical and isotopic characters i.e.the type of continental salinization and that of sea water origin.In the former type δ 18 O<-7 00‰, δ D<-55 0‰, 36 Cl/Cl>57±9(×10 -15 ) and 14 C ages are 1000~4000a(corrected).In the latter type δ 18 O and δ D are more than -7 00‰ and -55 0‰ respectively, δ 37 Cl approximates to the value of marine water and 14 C ages are more than 10 000a (corrected).The amount of sea water in saline water is more than 38 0%.
出处
《水文地质工程地质》
CAS
CSCD
1998年第3期4-8,共5页
Hydrogeology & Engineering Geology
基金
国家自然科学基金
关键词
河北平原
地下咸水
同位素组成
咸水
氧18
氧3
Hebei Plain, saline groundwater, isotopes( 18 O,D, 3H, 14 C, 36 Cl, 37 Cl)