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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ISSN1025-6016
1477-2639
1477-2639
DOI10.1080/10256016.2020.1857378

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Abstract 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.
AbstractList Radiocarbon (¹⁴C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the ¹⁴C content of dissolved inorganic carbon (¹⁴CDIC) 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 ¹⁴C-based groundwater age estimations and the corrections and errors that affect age determinations differently. Generally, the two factors that impact the results of ¹⁴C 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 ¹⁴C ages that depend on the water age. The cumulative impact of these errors substantively reduces the accuracy and confidence of ¹⁴C age determinations and corrections. When using ¹⁴C for groundwater age, consideration of both error types along with the use of samples having a range of ¹⁴CDIC contents helps practitioners recognize and minimize ¹⁴C age uncertainty, especially for groundwater ages of <1000 and >30,000 years B.P.
Radiocarbon (14C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14C content of dissolved inorganic carbon (14CDIC) 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 14C-based groundwater age estimations and the corrections and errors that affect age determinations differently. Generally, the two factors that impact the results of 14C 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 14C ages that depend on the water age. The cumulative impact of these errors substantively reduces the accuracy and confidence of 14C age determinations and corrections. When using 14C for groundwater age, consideration of both error types along with the use of samples having a range of 14CDIC contents helps practitioners recognize and minimize 14C age uncertainty, especially for groundwater ages of <1000 and >30,000 years B.P.Radiocarbon (14C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14C content of dissolved inorganic carbon (14CDIC) 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 14C-based groundwater age estimations and the corrections and errors that affect age determinations differently. Generally, the two factors that impact the results of 14C 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 14C ages that depend on the water age. The cumulative impact of these errors substantively reduces the accuracy and confidence of 14C age determinations and corrections. When using 14C for groundwater age, consideration of both error types along with the use of samples having a range of 14CDIC contents helps practitioners recognize and minimize 14C age uncertainty, especially for groundwater ages of <1000 and >30,000 years B.P.
Radiocarbon (14C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14C content of dissolved inorganic carbon (14CDIC) 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 14C-based groundwater age estimations and the corrections and errors that affect age determinations differently. Generally, the two factors that impact the results of 14C 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 14C ages that depend on the water age. The cumulative impact of these errors substantively reduces the accuracy and confidence of 14C age determinations and corrections. When using 14C for groundwater age, consideration of both error types along with the use of samples having a range of 14CDIC contents helps practitioners recognize and minimize 14C age uncertainty, especially for groundwater ages of <1000 and >30,000 years B.P.
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.
Author Han, Liang-Feng
Wassenaar, Leonard I.
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Snippet Radiocarbon ( 14 C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14 C content of dissolved...
Radiocarbon (14C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the 14C content of dissolved inorganic...
Radiocarbon (¹⁴C) is useful for estimating groundwater ages for transport and water resource exploitation assessment. If the ¹⁴C content of dissolved inorganic...
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SubjectTerms Age
Carbon 14
Carbon-13
Dissolved inorganic carbon
equations
Error correction
Groundwater
groundwater flow
isotope hydrology
natural radioactivity
Parameter estimation
Principles
radiocarbon dating
Resource evaluation
Resource exploitation
Uncertainty
water age
Water resources
Title Principles and uncertainties of 14C age estimations for groundwater transport and resource evaluation
URI https://www.tandfonline.com/doi/abs/10.1080/10256016.2020.1857378
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