Hydrology and Earth System Sciences
Hydrology and Earth System Sciences
HESS
Articles | Volume 28, issue 20
Articles | Volume 28, issue 20
https://doi.org/10.5194/hess-28-4755-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-28-4755-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 28, issue 20
Research article
 | 
29 Oct 2024
Research article |  | 29 Oct 2024

Experimental investigation of the interplay between transverse mixing and pH reaction in porous media

Adi Biran, Tomer Sapar, Ludmila Abezgauz, and Yaniv Edery

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

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) (27 Aug 2024) by Philippe Ackerer
AR by Yaniv Edery on behalf of the Authors (27 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (08 Sep 2024) by Philippe Ackerer
AR by Yaniv Edery on behalf of the Authors (08 Sep 2024)  Author's response   Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Yaniv Edery on behalf of the Authors (24 Oct 2024)   Author's adjustment   Manuscript
EA: Adjustments approved (28 Oct 2024) by Philippe Ackerer
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Short summary
In Earth sciences, pH-driven reactions in porous environments impact natural processes like mineral dissolution and groundwater remediation. Traditional models struggle due to pore-scale complexities. This study explores how porous structure and flow rate affect mixing and chemical reactions. Surprisingly, pH-driven reactions occur faster than predicted, emphasizing water’s unique pH behavior in porous media.
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