Articles | Volume 18, issue 12
https://doi.org/10.5194/hess-18-4951-2014
https://doi.org/10.5194/hess-18-4951-2014
Research article
 | 
09 Dec 2014
Research article |  | 09 Dec 2014

Using 14C and 3H to understand groundwater flow and recharge in an aquifer window

A. P. Atkinson, I. Cartwright, B. S. Gilfedder, D. I. Cendón, N. P. Unland, and H. Hofmann

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Short summary
This research article uses of radiogenic isotopes, stable isotopes and groundwater geochemistry to study groundwater age and recharge processes in the Gellibrand Valley, a relatively unstudied catchment and potential groundwater resource. The valley is found to contain both "old", regionally recharged groundwater (300-10,000 years) in the near-river environment, and modern groundwater (0-100 years old) further back on the floodplain. There is no recharge of the groundwater by high river flows.