Articles | Volume 18, issue 12
https://doi.org/10.5194/hess-18-5109-2014
https://doi.org/10.5194/hess-18-5109-2014
Research article
 | 
12 Dec 2014
Research article |  | 12 Dec 2014

Residence times and mixing of water in river banks: implications for recharge and groundwater–surface water exchange

N. P. Unland, I. Cartwright, D. I. Cendón, and R. Chisari

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (15 Jul 2014) by Mauro Giudici
AR by Nicolaas Unland on behalf of the Authors (18 Aug 2014)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (21 Aug 2014) by Mauro Giudici
RR by Anonymous Referee #2 (04 Sep 2014)
ED: Publish subject to minor revisions (Editor review) (08 Sep 2014) by Mauro Giudici
AR by Nicolaas Unland on behalf of the Authors (18 Sep 2014)  Author's response    Manuscript
ED: Publish as is (20 Sep 2014) by Mauro Giudici
AR by Nicolaas Unland on behalf of the Authors (29 Sep 2014)  Author's response    Manuscript
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Short summary
Periodic flooding of rivers should result in increased groundwater recharge near rivers and thus - younger and fresher groundwater near rivers. This study found the age and salinity of shallow groundwater to increase with proximity to the Tambo River in South East Australia. This appears to be due to the upwelling of older, regional groundwater closer the river. Other chemical parameters are consistent with this. This is a process that may be occurring in other similar river systems.