Field observations of soil hydrological flow path evolution over 10 millennia

Hartmann, Anne; Semenova, Ekaterina; Weiler, Markus; Blume, Theresa

doi:https://doi.org/10.5194/hess-24-3271-2020

Articles | Volume 24, issue 6

https://doi.org/10.5194/hess-24-3271-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Linking landscape organisation and hydrological functioning:...

https://doi.org/10.5194/hess-24-3271-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 24, issue 6

Research article

|

25 Jun 2020

Research article |

| 25 Jun 2020

Field observations of soil hydrological flow path evolution over 10 millennia

Anne Hartmann, Ekaterina Semenova, Markus Weiler, and Theresa Blume

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Final revised paper (published on 25 Jun 2020)
Preprint (discussion started on 24 Jan 2020)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of "Field observations of soil hydrological flow path evolution over 10 millenia"', Anonymous Referee #1, 21 Feb 2020
- AC1: 'Response to Reviewer 1', Anne Hartmann, 22 Mar 2020
RC2: 'comments on "Relevance and controls of preferential flow at the landscape scale"', Nicholas Jarvis, 05 Mar 2020
- AC2: 'Response to Reviewer 2', Anne Hartmann, 22 Mar 2020

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (further review by editor) (08 Apr 2020) by Patricia Saco

AR by Svenja Lange on behalf of the Authors (23 Apr 2020) Author's response Manuscript

ED: Publish as is (17 May 2020) by Patricia Saco

Short summary

Our field observation-based examination of flow path evolution, soil formation, and vegetation succession across 10 millennia shows how water flow paths and subsurface water storage are linked to the organization of evolving landscapes. The increase found in water storage and preferential flow paths with increasing soil age shows the effect of the complex interaction of vegetation and soil development on flow paths, water balance, and runoff formation during landscape evolution.