Articles | Volume 20, issue 9
https://doi.org/10.5194/hess-20-3581-2016
https://doi.org/10.5194/hess-20-3581-2016
Research article
 | 
06 Sep 2016
Research article |  | 06 Sep 2016

Using radon to understand parafluvial flows and the changing locations of groundwater inflows in the Avon River, southeast Australia

Ian Cartwright and Harald Hofmann

Viewed

Total article views: 2,662 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,476 1,073 113 2,662 98 83
  • HTML: 1,476
  • PDF: 1,073
  • XML: 113
  • Total: 2,662
  • BibTeX: 98
  • EndNote: 83
Views and downloads (calculated since 10 Sep 2015)
Cumulative views and downloads (calculated since 10 Sep 2015)

Cited

Saved (preprint)

Latest update: 06 Nov 2024
Download
Short summary
This paper uses the natural geochemical tracer Rn together with streamflow measurements to differentiate between actual groundwater inflows and water that exits the river, flows through the near-river sediments, and subsequently re-enters the river downstream (parafluvial flow). Distinguishing between these two components is important to understanding the water balance in gaining streams and in managing and protecting surface water resources.