Cosmogenic Ar dating is an emerging technique in dating mountain glacier ice, mapping ocean circulation, and tracing groundwater flow. We have realized an atom-trap system for the analysis of the radioactive isotope Ar (half-life = 269 years) in environmental samples. The system is capable of analyzing small (1-5 kg) environmental water or ice samples and achieves a count rate of 10 atoms/h for Ar at the modern isotopic abundance level of 8 × 10. By switching frequently between counting Ar atoms and measuring the stable and abundant isotope Ar, drift effects in the trapping efficiency are largely suppressed, leading to a more precise measurement of the isotope ratio Ar/Ar. Moreover, cleaning techniques are developed to alleviate cross-sample contamination, reducing the background Ar count rate down to <0.5 atoms/h. These advances allow us to determine the Ar age in the range of 250-1300 years with precisions of <20%.
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http://dx.doi.org/10.1063/5.0050620 | DOI Listing |
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