Articles | Volume 30, issue 6
https://doi.org/10.5194/hess-30-1675-2026
https://doi.org/10.5194/hess-30-1675-2026
Research article
 | 
30 Mar 2026
Research article |  | 30 Mar 2026

Elucidating loessal landslide initiation in wood- and shrub-land by hydro-mechanical heterogeneity

Ruijie Yang, Chao Ma, Xi Yang, Yan Zhang, Liqun Lyu, and Xinying Wang

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-6098', Anonymous Referee #1, 18 Jan 2026
    • AC1: 'Reply on RC1', Ruijie Yang, 28 Jan 2026
    • AC3: 'Reply on RC1', Ruijie Yang, 09 Feb 2026
  • RC2: 'Comment on egusphere-2025-6098', Anonymous Referee #2, 26 Jan 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (further review by editor) (12 Feb 2026) by Roberto Greco
AR by Ruijie Yang on behalf of the Authors (20 Feb 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (03 Mar 2026) by Roberto Greco
AR by Ruijie Yang on behalf of the Authors (09 Mar 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (10 Mar 2026) by Roberto Greco
AR by Ruijie Yang on behalf of the Authors (16 Mar 2026)
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Short summary

We carried out a series of field studies on woodland and shrubland slopes on China’s Loess Plateau. We found that woodland slopes allow water to move deeper into the ground, which helps them remain more stable, whereas shrubland slopes tend to hold more water near the surface and are more likely to fail. This means that landslides may play a bigger role in moving soil than previously thought, so soil loss on the Loess Plateau should be re-evaluated rather than linked only to surface runoff.

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