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《Journal of Glaciology and Geocryology》 2005-01
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Exchange of Groundwater and River Water in a Basin of the Middle Heihe River by Using δ~(18)O

ZHANG Ying-hua~(1), WU Yan-qing~(1), DING Jian-qiang~(2), WEN Xiao-hu~(1) (1.Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou Gansu 730000, China; 2.Gansu Province Transportation Planning, Survey and Design Institute, Lanzhou Gansu 730030,China)  
In arid regions of western China, water resources come from mountain watersheds and disappear in the desert plains. The exchange of surface water and groundwater takes place two or three times in a basin. It is essential to analyze the interaction between groundwater and surface water, so as to use water resources effectively and predict the change in the water environment. The conventional method of analysis, however, measures only the flow of a stream and cannot determine groundwater seepage accurately. Because of the distinct difference of {δ~(18)O} between groundwater and surface water, the method of using {{}~(18)O} was examined as an indicator for analyzing the interaction. With the addition of the mass balance equation, the composite proportion of different mixing components can be calculated. A conclusion was drawn from the computed result that, in the oases of the middle Heihe River, flood irrigation on vast farmlands has made a great impact on the transform between groundwater and surface water. The irrational irrigation has caused some problems, such as environmental deterioration and land subsidence.
【Fund】: 国家自然科学基金重大研究计划项目(90102003);; 中国科学院知识创新工程重大项目(KZCX1 10 03);; 2000年教育部科学技术研究重点项目(00233)资助
【CateGory Index】: P641.3
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