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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Published in: | Applied radiation and isotopes Vol. 126; no. C |
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Main Authors: | , , , , , , , , , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
United States
Elsevier
01-08-2017
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Subjects: | |
Online Access: | Get full text |
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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. |
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Bibliography: | PNNL-SA-121026 USDOE AC05-76RL01830 |
ISSN: | 0969-8043 1872-9800 |
DOI: | 10.1016/j.apradiso.2016.12.037 |