Articles | Volume 26, issue 21
Hydrol. Earth Syst. Sci., 26, 5515–5534, 2022
https://doi.org/10.5194/hess-26-5515-2022
Hydrol. Earth Syst. Sci., 26, 5515–5534, 2022
https://doi.org/10.5194/hess-26-5515-2022
Research article
07 Nov 2022
Research article | 07 Nov 2022

Effects of passive-storage conceptualization on modeling hydrological function and isotope dynamics in the flow system of a cockpit karst landscape

Guangxuan Li 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 hess-2021-492', Anonymous Referee #1, 21 Feb 2022
    • AC1: 'Reply on RC1', Guangxuan Li, 05 May 2022
  • RC2: 'Comment on hess-2021-492', Catherine Bertrand, 14 Jun 2022
    • AC2: 'Reply on RC2', Guangxuan Li, 11 Jul 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (16 Jul 2022) by Thom Bogaard
AR by Guangxuan Li on behalf of the Authors (26 Aug 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (30 Aug 2022) by Thom Bogaard
RR by Anonymous Referee #1 (08 Sep 2022)
RR by Catherine Bertrand (28 Sep 2022)
ED: Publish subject to minor revisions (review by editor) (07 Oct 2022) by Thom Bogaard
AR by Guangxuan Li on behalf of the Authors (14 Oct 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (14 Oct 2022) by Thom Bogaard
AR by Guangxuan Li on behalf of the Authors (17 Oct 2022)  Author's response    Manuscript
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Short summary
We developed a coupled flow–tracer model to understand the effects of passive storage on modeling hydrological function and isotope dynamics in a karst flow system. Models with passive storages show improvement in matching isotope dynamics performance, and the improved performance also strongly depends on the number and location of passive storages. Our results also suggested that the solute transport is primarily controlled by advection and hydrodynamic dispersion in the steep hillslope unit.