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《Journal of Jilin University(Earth Science Edition)》 2007-02
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Application of Inverse Geochemical Modeling in the Correction of Groundwater ~(14)C Dating:advances and Thoughts

SU Xiao-si1,LIN Xue-yu1,2,DONG Wei-hong1, WAN Yu-yu1 1.Institute of Water Resources and Environment,Jilin University,Changchun 130026,China 2.College of Water Sciences,Beijing Normal University,Beijing 100875,China  
Correction of groundwater 14C dating is the hot spot in the research on groundwater dating.The coupling of inverse geochemical reaction path model and isotope mass transfer model can be completely involved in the effects of different carbon sources and different hydrogeochemical reactions on 14C mass transfer,which has made the correction technique of groundwater 14C dating in a new state.Identification of the main factors and their extent affecting the concentration of 14C in the groundwater evolution is of high importance for the accuracy and reliability of groundwater 14C age correction result.The specific character of recharge environment and the removal of non-possible solutions should be paid more attention in application of inverse geochemical modeling in the correction of groundwater 14C da-ting.
【Fund】: 教育部博士点基金项目(20030027020);; 国家重点基础研究发展规划(973)项目(G1999043606);; 中国国土资源大调查项目(1212010331302);; 吉林大学“985”计划;; 教育部城市环境与可持续发展联合研究中心吉林大学分中心资助;; 水资源与水环境重点实验室(原地质矿产部水资源评价与管理系列模型开放研究实验室)资助
【CateGory Index】: P641.3
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