Dating of groundwater, ocean water and glacier ice with noble gas radioisotopes
Ice Sampling
Dr. Florian Ritterbusch
INF 229, SR 108/110

The noble gas radioisotopes 81Kr (t1/2 =229 ka), 85Kr (t1/2 =1 1 a) and 39Ar (t1/2 =268 a) are valuable dating tools for groundwater, ocean water and glacier ice, serving applications such as drinking water management, oc ean current tracing and climate reconstruction. Together with 14C, these radioisotopes cover an age range from present back to 1.3 million years. Due to their extremely low environmental abundances (10-17 …10-11 ) corresponding to only a few thousand atoms per kilogram of water or ice, their detection is very challenging and in the case of 81 Kr, has practically not been possible in the past.
In the recent two decades, the laser based method Atom Trap Trace Analysis (ATTA), which detects single atoms via their fluorescence in a magneto optical trap, has succeeded in measuring these radioisotopes on natural levels. Initially, tons of water or ice were necessary for ATTA, which severely hampered its use for dating of environmental samples. Due to progress in the ATTA instruments, the sample size could be lowered to ~10 kg of water or ice, allowing for applications such as dating of deep water from the Pacific Ocean and ice cores from Antarctica and Tibet.
In this colloquium I will present an overview of the ATTA method, recen t dating results on groundwater, ocean wate r and glacier ice as well as the latest advances towards 81Kr and 39Ar dating with 1 kg of water or ice.


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J. Q. Gu et al. (2022), Estimation of the Ventilation Transit Time Distribution at the Yap Mariana Junction Using 39Ar, 85Kr and 14C Tracers, JGR Oceans

D.E. Martínez , et al. ( 2022), 81Kr reveals one million year old groundwater at the Atlantic coast of Argentina as a record of Mid Pleistocene climate, Journal of Hydrology

Ritterbusch et al (2022), A Tibetan ice core covering the past 1,300 years radiometrically datedwith 39Ar, Proceedings of the National Academy of Sciences