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Chemical and Isotopic Constraints on 14C Dating of Groundwater

  • Fontes J
Springer New York, (1992), 242-261
DOI: 10.1007/978-1-4757-4249-7_17
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Abstract

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.

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Fontes, J.-C. (1992). Chemical and Isotopic Constraints on 14C Dating of Groundwater. In Radiocarbon After Four Decades (pp. 242–261). Springer New York. https://doi.org/10.1007/978-1-4757-4249-7_17

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