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《Journal of Jilin University(Earth Science Edition)》 2011-04
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Comparison of ~4He and ~(14)C Dating of Groundwater from Quaternary Confined Aquifers in Hebei Plain

WEI Wen,CHEN Zong-yu,ZHAO Hong-mei,LIU Jun,WANG YingInstitute of Hydrogeology and Environmental Geology,Chinese Academy of Geological Sciences,Shijiazhuang 050061,China  
4He isotope is an ideal tracer for groundwater dating,but it was generally disagreement with 14C dating results due to dating scales and multisources.By taking noble gas samples and 14C samples in the same well from the Quaternary aquifers in Hebei Plain,the results revealed that the concentrations of radiogenic 4Herad components ranged from 5.43×10-8 to 8 994×10-8 cm3·STP/g by using closed-system equilibration(CE) model.Furthermore,it was found that 4He age of groundwater ranged from 8.8 to 55.9 ka and 14C age ranged from 7.7 to 35.2 ka,which indicated that above two results differed slightly and correspondingly we can concluded that the application of 4He dating in Hebei Plain is reasonable.
【Fund】: 国家“973”计划项目(2010CB428803);; 水文地质环境地质研究所基本科研项目(SK200814)
【CateGory Index】: P641.3
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