Abstract: Dissolved Kr and Xe isotope ratios in groundwater enable quantitative resolution of water-table depth at the time of recharge (AGU Fall Meeting 2018)

Dissolved Kr and Xe isotope ratios in groundwater enable quantitative resolution of water-table depth at the time of recharge

Alan M Seltzer¹, Wesley R Danskin², Riley Gannon³, Jessica Yi-Jun Ng¹, Justin T Kulongoski⁴, Martin Stute⁵ and Jeffrey P Severinghaus⁶, (1)Scripps Institution of Oceanography, La Jolla, CA, United States, (2)U.S. Geological Survey, San Diego, CA, United States, (3)U.S. Geological Survey, San Diego, United States, (4)Scripps Institution of Oceanography, Geosciences Research Division, La Jolla, United States, (5)Barnard College, New York, NY, United States, (6)Scripps Institution of Oceanography, La Jolla, United States

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