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《Geological Science and Technology Information》 2009-06
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Features of Environmental Isotopes of Hydrogen and Oxygen of Water and Their Indication in Yanqi Basin,China

LIU Yan-feng1,JIANG Gui-rong1,JIN Meng-gui1,LI Xu-feng2(1.School of Environmental Studies,China University of Geosciences,Wuhan 430074,China;2.Center for Hydrogeology and Environmental Geology,CGS,Baoding Hebei 071051,China)  
Based on the environmental isotope features of hydrogen and oxygen and deuterium excess(d) of groundwater and Kaidu River in Yanqi Basin,this paper analyses the spatial characteristics of D、18O and d in different water,which may indicate the main sources of groundwater and the interaction between groundwater and Kaidu River according to the D vs.18O graph.The D varies from-87.60‰ to-61.82‰ and the 18O,from-10.90‰ to-9.73‰ in groundwater.While the D ranges from-71.95‰ to-58.58‰ and the 18O,from-9.57‰ to-8.64‰ in stream water.The results indicate that the groundwater and stream water are mainly derived from the snow melting water and rainfall,and the source water is evaporated a long time before the water infiltration to the groundwater.There is a leak interaction between groundwater and surface water.The groundwater in deep aquifer is mainly recharged by the intensive infiltration of stream water in the proluvial fan,and the groundwater in shallow aquifer mainly derives from irrigation water derived from Kaidu River in plain area.The groundwater in porous Quaternary formation can be regarded as one whole groundwater system because of the close interaction between groundwater and surface water.
【Fund】: 国家重点基础研究发展计划项目(2007CB416604);; 国家自然科学基金项目(40472123;40302056)
【CateGory Index】: P641.3
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