Chemical and Isotopic Constraints on 14C Dating of Groundwater

  • Jean-Charles Fontes


The conversion of the 14C activity of the total dissolved inorganic carbon (TDIC) in terms of groundwater residence time is an interpretation requiring the discussion of several constraints. This chapter is a review of some geochemical conditions that must be considered for groundwater dating.


Unsaturated Zone Isotope Exchange Accelerator Mass Spectrometry Water Resource Research Solid Carbonate 


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© Springer Science+Business Media New York 1992

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  • Jean-Charles Fontes

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