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

Viewed

Total article views: 4,660 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,761 2,788 111 4,660 87 82
  • HTML: 1,761
  • PDF: 2,788
  • XML: 111
  • Total: 4,660
  • BibTeX: 87
  • EndNote: 82
Views and downloads (calculated since 06 Jun 2014)
Cumulative views and downloads (calculated since 06 Jun 2014)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 21 Nov 2024
Download
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.