Principles and uncertainties of 14C age estimations for groundwater transport and resource evaluation

Radiocarbon ( 14 C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14 C content of dissolved inorganic carbon ( 14 C DIC ) is known, the age of groundwater can be estimated by applying a radiocarbon decay equation combined with an appropria...

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Published inIsotopes in environmental and health studies Vol. 57; no. 2; pp. 111 - 141
Main Authors Han, Liang-Feng, Wassenaar, Leonard I.
Format Journal Article
LanguageEnglish
Published Amsterdam Taylor & Francis 01.05.2021
Taylor & Francis Ltd
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Summary:Radiocarbon ( 14 C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14 C content of dissolved inorganic carbon ( 14 C DIC ) is known, the age of groundwater can be estimated by applying a radiocarbon decay equation combined with an appropriate geochemical correction model. However, age determinations are subject to uncertainties caused by parameters which need to be estimated or assumed. Here, we discuss the principles of 14 C-based groundwater age estimations and the corrections and errors that affect age determinations differently. Generally, the two factors that impact the results of 14 C groundwater age are Type-1 and Type-2 errors. Type-1 errors are pulse-type changes on derived groundwater ages that are independent of the water age. Type-2 errors cause gradual changes on derived groundwater 14 C ages that depend on the water age. The cumulative impact of these errors substantively reduces the accuracy and confidence of 14 C age determinations and corrections. When using 14 C for groundwater age, consideration of both error types along with the use of samples having a range of 14 C DIC contents helps practitioners recognize and minimize 14 C age uncertainty, especially for groundwater ages of <1000 and >30,000 years B.P.
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ISSN:1025-6016
1477-2639
1477-2639
DOI:10.1080/10256016.2020.1857378