Setting a Limit on Anthropogenic Sources of Atmospheric 81Kr through Atom Trap Trace Analysis
J. C. Zappala (1, 2), K. Bailey (1), W. Jiang (3), B. Micklich (1),, P. Mueller (1), T. P. O'Connor (1), R. Purtschert (4) ((1) Argonne National, Laboratory, (2) University of Chicago, (3) University of Science and, Technology of China, (4) University of Bern)

TL;DR
This paper establishes a 2.5% upper limit on human-made 81Kr in the atmosphere using advanced laser-based atom counting, enhancing the reliability of 81Kr dating for earth sciences.
Contribution
It introduces a precise measurement of anthropogenic 81Kr contribution, improving the accuracy of 81Kr dating methods in geoscience research.
Findings
Anthropogenic 81Kr contribution limited to 2.5% at 90% confidence
Achieved 1% relative uncertainty in 81Kr/Kr measurements
Removed a systematic constraint for 81Kr dating
Abstract
We place a 2.5% limit on the anthropogenic contribution to the modern abundance of 81Kr/Kr in the atmosphere at the 90% confidence level. Due to its simple production and transport in the terrestrial environment, 81Kr (halflife = 230,000 yr) is an ideal tracer for old water and ice with mean residence times in the range of 10^5-10^6 years. In recent years, 81Kr-dating has been made available to the earth science community thanks to the development of Atom Trap Trace Analysis (ATTA), a laser-based atom counting technique. Further upgrades and improvements to the ATTA technique now allow us to demonstrate 81Kr/Kr measurements with relative uncertainties of 1% and place this new limit on anthropogenic 81Kr. As a result of this limit, we have removed a potential systematic constraint for 81Kr-dating.
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Taxonomy
TopicsRadioactive contamination and transfer · Geology and Paleoclimatology Research · Isotope Analysis in Ecology
