Articles | Volume 26, issue 13
https://doi.org/10.5194/hess-26-3359-2022
https://doi.org/10.5194/hess-26-3359-2022
Research article
 | 
05 Jul 2022
Research article |  | 05 Jul 2022

Experimental study of non-Darcy flow characteristics in permeable stones

Zhongxia Li, Junwei Wan, Tao Xiong, Hongbin Zhan, Linqing He, and Kun Huang

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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-2021-588', Anonymous Referee #1, 11 Dec 2021
    • AC1: 'Reply on RC1', Hongbin Zhan, 12 Feb 2022
  • RC2: 'Comment on hess-2021-588', Anonymous Referee #2, 16 Jan 2022
    • AC2: 'Reply on RC2', Hongbin Zhan, 12 Feb 2022

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) (28 Feb 2022) by Jorge Isidoro
AR by Hongbin Zhan on behalf of the Authors (01 Mar 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (07 Apr 2022) by Jorge Isidoro
AR by Hongbin Zhan on behalf of the Authors (14 Apr 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (04 May 2022) by Jorge Isidoro
ED: Publish as is (01 Jun 2022) by Thom Bogaard (Executive editor)
AR by Hongbin Zhan on behalf of the Authors (02 Jun 2022)  Manuscript 
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Short summary
Four permeable rocks with different pore sizes were considered to provide experimental evidence of Forchheimer flow and the transition between different flow regimes. The mercury injection technique was used to measure the pore size distribution, which is an essential factor for determining the flow regime, for four permeable stones. Finally, the influences of porosity and particle size on the Forchheimer coefficients were discussed.