An atom trap system for 39Ar dating with improved precision

Cosmogenic 39Ar 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 39Ar (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 39Ar at the modern isotopic abundance level of 8 × 10−16. By switching frequently between counting 39Ar atoms and measuring the stable and abundant isotope 38Ar, drift effects in the trapping efficiency are largely suppressed, leading to a more precise measurement of the isotope ratio 39Ar/38Ar. Moreover, cleaning techniques are developed to alleviate cross-sample contamination, reducing the background 39Ar count rate down to