Articles | Volume 21, issue 6
Hydrol. Earth Syst. Sci., 21, 3105–3123, 2017
https://doi.org/10.5194/hess-21-3105-2017
Hydrol. Earth Syst. Sci., 21, 3105–3123, 2017
https://doi.org/10.5194/hess-21-3105-2017

Research article 29 Jun 2017

Research article | 29 Jun 2017

Electrical resistivity dynamics beneath a fractured sedimentary bedrock riverbed in response to temperature and groundwater–surface water exchange

Colby M. Steelman et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by Editor and Referees) (12 Feb 2017) by Mauro Giudici
AR by Colby Steelman on behalf of the Authors (10 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (19 Mar 2017) by Mauro Giudici
RR by Anonymous Referee #1 (29 Mar 2017)
RR by Anonymous Referee #3 (13 Apr 2017)
ED: Publish subject to minor revisions (further review by Editor) (28 Apr 2017) by Mauro Giudici
AR by Colby Steelman on behalf of the Authors (04 May 2017)  Author's response    Manuscript
ED: Publish as is (27 May 2017) by Mauro Giudici
Download
Short summary
The Eramosa River flows along a fractured sedimentary bedrock aquifer with large subsurface channel features. This study examines the potential for groundwater–surface water exchange beneath the fractured bedrock riverbed and the impacts of seasonal and intraseasonal flow system transience on the geoelectrical properties of the rock. Our results will have implications to the conceptual understanding of groundwater–surface water interaction within fractured bedrock river environments.