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《Geoscience》 2014-06
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Using the ~3H and ~(14)C Dating Methods to Calculate the Groundwater Age in Nuomuhong,Qaidam Basin

LIU Feng;CUI Ya-li;ZHANG Ge;GENG Fu-qiang;LIU Jie;School of Water Resources and Environment,China University of Geosciences;The Institute of Hydrogeology and Environment Geology,Chinese Academy of Geological Sciences;Xi'an Center of Geological Survey,China Geological Survey;  
By utilizing the3 H and14C dating methods,this paper calculated the distribution of groundwater age and then analyzed the groundwater renewability in the study area of Nuomuhong in Qaidam basin.The results show that:(1) in areas from the mountain to the middle part of the alluvial-proluvial fan,the groundwater age varies slightly(15-18 a),indicating that the groundwater is recharged after 1952 with a strong renewability;(2) the groundwater age,in the leading edge of the alluvial-proluvial fan,is less than 2 ka,indicating that the groundwater is a mixture of the modern groundwater with the fossil groundwater and has a poor renewability;(3) in areas from overflow zone to the center of the basin,the groundwater age gets older rapidly from 5 ka to28 ka,indicating that the hidden fault underlaid the overflow zone has the property of water blocking,and that groundwater in this area can be considered as unrenewable resources.
【Fund】: 中国地质调查局干旱—半干旱区地下水与生态重点实验室开放基金项目;; 中国地质调查局工作项目“柴达木盆地循环经济试验区水文地质环境地质调查”(1212011220974)
【CateGory Index】: P641;P597.3
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