Articles | Volume 21, issue 4
https://doi.org/10.5194/hess-21-2249-2017
https://doi.org/10.5194/hess-21-2249-2017
Research article
 | 
02 May 2017
Research article |  | 02 May 2017

Variation of soil hydraulic properties with alpine grassland degradation in the eastern Tibetan Plateau

Tao Pan, Shuai Hou, Shaohong Wu, Yujie Liu, Yanhua Liu, Xintong Zou, Anna Herzberger, and Jianguo Liu

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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 (further review by Editor and Referees) (23 Oct 2016) by Lixin Wang
AR by Tao Pan on behalf of the Authors (25 Oct 2016)
ED: Publish subject to revisions (further review by Editor and Referees) (30 Oct 2016) by Lixin Wang
ED: Referee Nomination & Report Request started (29 Nov 2016) by Lixin Wang
RR by Anonymous Referee #1 (26 Dec 2016)
RR by Anonymous Referee #2 (02 Jan 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (11 Jan 2017) by Lixin Wang
AR by Tao Pan on behalf of the Authors (22 Feb 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (24 Feb 2017) by Lixin Wang
RR by Anonymous Referee #2 (28 Feb 2017)
RR by Anonymous Referee #1 (21 Mar 2017)
ED: Publish subject to minor revisions (further review by Editor) (22 Mar 2017) by Lixin Wang
AR by Tao Pan on behalf of the Authors (31 Mar 2017)  Manuscript 
ED: Publish as is (04 Apr 2017) by Lixin Wang
AR by Tao Pan on behalf of the Authors (06 Apr 2017)
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Short summary
This study shows that soil hydraulic properties, especially those of the top soil, varied greatly with alpine swamp meadow degradation. Soil porosity is the dominant influencing factor of soil hydraulic properties. The results suggest that alpine swamp meadow degradation would inevitably lead to negative hydrological effects. Hydrological modelling in the Tibetan Plateau and similar regions are recommended to understand the effects of degradation on soil hydraulic properties.