Articles | Volume 7, issue 2
https://doi.org/10.5194/soil-7-563-2021
https://doi.org/10.5194/soil-7-563-2021
Original research article
 | 
30 Aug 2021
Original research article |  | 30 Aug 2021

Hydrological soil properties control tree regrowth after forest disturbance in the forest steppe of central Mongolia

Florian Schneider, Michael Klinge, Jannik Brodthuhn, Tino Peplau, and Daniela Sauer

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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: Revision (21 Dec 2020) by Nikolaus J. Kuhn
AR by Florian Schneider on behalf of the Authors (27 Jan 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Reconsider after major revisions (05 Mar 2021) by Nikolaus J. Kuhn
AR by Florian Schneider on behalf of the Authors (06 Mar 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (18 Mar 2021) by Nikolaus J. Kuhn
RR by Anonymous Referee #3 (20 Jul 2021)
ED: Publish as is (29 Jul 2021) by Nikolaus J. Kuhn
ED: Publish as is (04 Aug 2021) by Kristof Van Oost (Executive editor)
AR by Florian Schneider on behalf of the Authors (05 Aug 2021)  Author's response   Manuscript 
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Short summary
The central Mongolian forest steppe underlies a recent decline of forested area. We analysed the site and soil properties in the Khangai Mountains to identify differences between disturbed forest areas with and without regrowth of trees. More silty soils were found under areas with tree regrowth and more sandy soils under areas without tree regrowth. Due to the continental, semi-arid climate, soil properties which increase the amount of available water are decisive for tree regrowth in Mongolia.