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张掖盆地东段“三水”转化同位素特征
引用本文:崔振卿,杨丽萍,赵艳娜.张掖盆地东段“三水”转化同位素特征[J].水资源保护,2007,23(4):15-17.
作者姓名:崔振卿  杨丽萍  赵艳娜
作者单位:甘肃省地质矿产勘查开发局水文地质工程地质勘察院,甘肃,张掖,734000
基金项目:中国地质调查局区域地质调查项目
摘    要:利用传统手段与环境同位素技术结合的方法,以水源地建设为例,分析研究了张掖盆地东段地下水资源的可更新性,揭示了水源地及其外围地下水含水层系统之间的补、径、排条件,初步分析了地下水水流系统,由此得出结论:深层承压水越流补给浅层水,同时也是泉水的主要来源。

关 键 词:地下水  含水层  深层承压水  环境同位素
文章编号:1004-6933(2007)04-0015-03
收稿时间:2006-08-15
修稿时间:2006-08-15

Isotope characteristics of transformation of three kinds of waters in East Zhangye Basin
CUI Zhen-qing,YANG Li-ping,ZHAO Yan-na.Isotope characteristics of transformation of three kinds of waters in East Zhangye Basin[J].Water Resources Protection,2007,23(4):15-17.
Authors:CUI Zhen-qing  YANG Li-ping  ZHAO Yan-na
Affiliation:Institute of Hydrogeology and Engineering Geology, Gansu Provincial Bureau of Geology and Mineral Exploration and Development, Zhangye 734000, China
Abstract:Taking the construction of water source regions as an example,the renewal of the groundwater in East Zhangye Basin was studied using the method combining the traditional method with environment isotope technology.The conditions of water recharge,runoff and draining between the water source and its surrounding groundwater aquifer were discussed,and the groundwater fluid system was analyzed briefly.It is concluded that the deep confined water supplies the shallow water,and it's also the main sources of spring water.
Keywords:ground water  aquifer  deep confined water  environmental isotope
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