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

Abstract

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. Lastly, we present the methods employed for arriving at an age-date for a given sample of argon degassed from groundwater.

Authors:
 [1];  [1];  [1];  [1];  [1];  [1];  [1];  [2];  [1];  [1];  [1];  [1];  [1];  [1]
  1. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
  2. U.S.G.S. California Water Science Center, San Diego, CA (United States)
Publication Date:
Research Org.:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1343946
Alternate Identifier(s):
OSTI ID: 1550640
Report Number(s):
PNNL-SA-117389
Journal ID: ISSN 0969-8043; PII: S0969804316306509
Grant/Contract Number:  
AC05-76RL01830; PNNL-SA-121026
Resource Type:
Accepted Manuscript
Journal Name:
Applied Radiation and Isotopes
Additional Journal Information:
Journal Volume: 126; Journal ID: ISSN 0969-8043
Publisher:
Elsevier
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; 58 GEOSCIENCES; Argon-39; age-dating; groundwater; ultra-low-background; proportional counting

Citation Formats

Mace, Emily, Aalseth, Craig, Brandenberger, Jill, Day, Anthony, Hoppe, Eric, Humble, Paul, Keillor, Martin, Kulongoski, Justin, Overman, Cory, Panisko, Mark, Seifert, Allen, White, Signe, Freeburg, Eric Wilcox, and Williams, Richard. Methods for using argon-39 to age-date groundwater using ultra-low-background proportional counting. United States: N. p., 2016. Web. doi:10.1016/J.APRADISO.2016.12.037.
Mace, Emily, Aalseth, Craig, Brandenberger, Jill, Day, Anthony, Hoppe, Eric, Humble, Paul, Keillor, Martin, Kulongoski, Justin, Overman, Cory, Panisko, Mark, Seifert, Allen, White, Signe, Freeburg, Eric Wilcox, & Williams, Richard. Methods for using argon-39 to age-date groundwater using ultra-low-background proportional counting. United States. https://doi.org/10.1016/J.APRADISO.2016.12.037
Mace, Emily, Aalseth, Craig, Brandenberger, Jill, Day, Anthony, Hoppe, Eric, Humble, Paul, Keillor, Martin, Kulongoski, Justin, Overman, Cory, Panisko, Mark, Seifert, Allen, White, Signe, Freeburg, Eric Wilcox, and Williams, Richard. Wed . "Methods for using argon-39 to age-date groundwater using ultra-low-background proportional counting". United States. https://doi.org/10.1016/J.APRADISO.2016.12.037. https://www.osti.gov/servlets/purl/1343946.
@article{osti_1343946,
title = {Methods for using argon-39 to age-date groundwater using ultra-low-background proportional counting},
author = {Mace, Emily and Aalseth, Craig and Brandenberger, Jill and Day, Anthony and Hoppe, Eric and Humble, Paul and Keillor, Martin and Kulongoski, Justin and Overman, Cory and Panisko, Mark and Seifert, Allen and White, Signe and Freeburg, Eric Wilcox and Williams, Richard},
abstractNote = {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. Lastly, we present the methods employed for arriving at an age-date for a given sample of argon degassed from groundwater.},
doi = {10.1016/J.APRADISO.2016.12.037},
journal = {Applied Radiation and Isotopes},
number = ,
volume = 126,
place = {United States},
year = {Wed Dec 21 00:00:00 EST 2016},
month = {Wed Dec 21 00:00:00 EST 2016}
}

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