Articles | Volume 19, issue 3
Biogeosciences, 19, 877–889, 2022
https://doi.org/10.5194/bg-19-877-2022
Biogeosciences, 19, 877–889, 2022
https://doi.org/10.5194/bg-19-877-2022

Research article 11 Feb 2022

Research article | 11 Feb 2022

Isotopic differences in soil–plant–atmosphere continuum composition and control factors of different vegetation zones on the northern slope of the Qilian Mountains

Yuwei Liu et al.

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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 bg-2021-127', Anonymous Referee #1, 17 Jun 2021
  • RC2: 'Comment on bg-2021-127', Anonymous Referee #2, 13 Jul 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (22 Aug 2021) by Aninda Mazumdar
AR by Guofeng Zhu on behalf of the Authors (26 Aug 2021)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Sep 2021) by Aninda Mazumdar
RR by Anonymous Referee #2 (02 Oct 2021)
ED: Reconsider after major revisions (11 Oct 2021) by Aninda Mazumdar
AR by Guofeng Zhu on behalf of the Authors (18 Oct 2021)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (09 Nov 2021) by Aninda Mazumdar
AR by Guofeng Zhu on behalf of the Authors (14 Nov 2021)  Author's response
ED: Publish as is (15 Dec 2021) by Aninda Mazumdar
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Short summary
We took the water cycle process of soil–plant–atmospheric precipitation as the research objective. In the water cycle of soil–plant–atmospheric precipitation, precipitation plays the main controlling role. The main source of replenishment for alpine meadow plants is precipitation and alpine meltwater; the main source of replenishment for forest plants is soil water; and the plants in the arid foothills mainly use groundwater.
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