Methods for using argon-39 to age-date groundwater using ultra-low-background proportional counting

Argon-39 can be used as a tracer for age-dating glaciers, oceans, and more recently, groundwater. With a half-life of 269 years, 39Ar fills an intermediate age range gap (50-1,000 years) not currently covered by other common groundwater tracers. Therefore, adding this tracer to the data suite for gr...

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Bibliographic Details
Published in:Applied radiation and isotopes Vol. 126; no. C
Main Authors: Mace, Emily, Aalseth, Craig, Brandenberger, Jill, Day, Anthony, Hoppe, Eric, Humble, Paul, Keillor, Martin, Kulongoski, Justin, Overman, Cory, Panisko, Mark, Seifert, Allen, White, Signe, Wilcox Freeburg, Eric, Williams, Richard
Format: Journal Article
Language:English
Published: United States Elsevier 01-08-2017
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Summary:Argon-39 can be used as a tracer for age-dating glaciers, oceans, and more recently, groundwater. With a half-life of 269 years, 39Ar fills an intermediate age range gap (50-1,000 years) not currently covered by other common groundwater tracers. Therefore, adding this tracer to the data suite for groundwater studies provides an important tool for improving our understanding of groundwater systems. We present the methods employed for arriving at an age-date for a given sample of argon degassed from groundwater.
Bibliography:PNNL-SA-121026
USDOE
AC05-76RL01830
ISSN:0969-8043
1872-9800
DOI:10.1016/j.apradiso.2016.12.037