Articles | Volume 20, issue 9
https://doi.org/10.5194/hess-20-3873-2016
https://doi.org/10.5194/hess-20-3873-2016
Research article
 | 
20 Sep 2016
Research article |  | 20 Sep 2016

Exploring water cycle dynamics by sampling multiple stable water isotope pools in a developed landscape in Germany

Natalie Orlowski, Philipp Kraft, Jakob Pferdmenges, and Lutz Breuer

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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 (18 Dec 2015) by Markus Weiler
AR by Natalie Orlowski on behalf of the Authors (14 Jan 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (17 Jan 2016) by Markus Weiler
RR by Anonymous Referee #1 (29 Jan 2016)
RR by Anonymous Referee #2 (04 Mar 2016)
ED: Reconsider after major revisions (07 Apr 2016) by Markus Weiler
AR by Natalie Orlowski on behalf of the Authors (02 Jun 2016)  Author's response   Manuscript 
ED: Reconsider after major revisions (28 Jun 2016) by Markus Weiler
ED: Referee Nomination & Report Request started (29 Jun 2016) by Markus Weiler
RR by Anonymous Referee #2 (07 Jul 2016)
ED: Publish subject to minor revisions (Editor review) (07 Jul 2016) by Markus Weiler
AR by Natalie Orlowski on behalf of the Authors (17 Jul 2016)  Author's response   Manuscript 
ED: Publish subject to minor revisions (Editor review) (20 Jul 2016) by Markus Weiler
AR by Natalie Orlowski on behalf of the Authors (27 Jul 2016)  Author's response   Manuscript 
ED: Publish as is (16 Aug 2016) by Markus Weiler
AR by Natalie Orlowski on behalf of the Authors (17 Aug 2016)
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Short summary
The 2-year measurements of δ2H and δ18O in rainfall, stream, soil, and groundwater revealed that surface and groundwater are isotopically disconnected from the annual precipitation cycle but showed bidirectional interactions in the Schwingbach catchment. We established a hydrological model to estimate spatially distributed groundwater ages and flow directions. Our model revealed complex age dynamics and showed that runoff must have been stored in the catchment for much longer than event water.