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 in | Isotopes in environmental and health studies Vol. 57; no. 2; pp. 111 - 141 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Amsterdam
Taylor & Francis
01.05.2021
Taylor & Francis Ltd |
Subjects | |
Online Access | Get full text |
ISSN | 1025-6016 1477-2639 1477-2639 |
DOI | 10.1080/10256016.2020.1857378 |
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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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StartPage | 111 |
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 |
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