Thermal non-equilibrium of porous flow in a resting matrix applicable to melt migration: a parametric study

Chevalier, Laure; Schmeling, Harro

doi:https://doi.org/10.5194/se-13-1045-2022

Articles | Volume 13, issue 6

https://doi.org/10.5194/se-13-1045-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/se-13-1045-2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 13, issue 6

Research article

|

27 Jun 2022

Research article |

| 27 Jun 2022

Thermal non-equilibrium of porous flow in a resting matrix applicable to melt migration: a parametric study

Laure Chevalier and Harro Schmeling

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Final revised paper (published on 27 Jun 2022)
Supplement to the final revised paper
Preprint (discussion started on 21 Dec 2021)
Supplement to the preprint

Interactive discussion

Status: closed

RC1:
'Comment on se-2021-149', John Rudge, 12 Jan 2022

See PDF.

Citation: https://doi.org/10.5194/se-2021-149-RC1
- AC1: 'Reply on RC1', Harro Schmeling, 04 Mar 2022
  
  Please see the attached authors' comments
  
  Citation: https://doi.org/10.5194/se-2021-149-AC1
RC2:
'Comment on se-2021-149', Cian Wilson, 24 Jan 2022

See pdf.

Citation: https://doi.org/10.5194/se-2021-149-RC2
- AC2: 'Reply on RC2', Harro Schmeling, 04 Mar 2022
  
  Please see the attached authors' comments
  
  Citation: https://doi.org/10.5194/se-2021-149-AC2
EC1: 'Comment on se-2021-149', Juliane Dannberg, 07 Feb 2022

Dear Laure Chevalier and Harro Schmeling,
Both reviewers have raised concerns about the analysis and presentation of the results in the manuscript, and they have made some good points on how these could be improved. Please address these points in your final response.
Best,

Juliane Dannberg

Citation: https://doi.org/10.5194/se-2021-149-EC1

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload

AR by Harro Schmeling on behalf of the Authors (04 Mar 2022) Author's response Manuscript

EF by Polina Shvedko (07 Mar 2022) Author's tracked changes

ED: Referee Nomination & Report Request started (23 Mar 2022) by Juliane Dannberg

RR by Samuel Butler (30 Apr 2022)

RR by Cian Wilson (09 May 2022)

ED: Publish subject to technical corrections (16 May 2022) by Juliane Dannberg

ED: Publish subject to minor revisions (review by editor) (16 May 2022) by Susanne Buiter (Executive editor)

AR by Harro Schmeling on behalf of the Authors (27 May 2022) Author's response Author's tracked changes Manuscript

ED: Publish as is (07 Jun 2022) by Juliane Dannberg

ED: Publish as is (07 Jun 2022) by Susanne Buiter (Executive editor)

AR by Harro Schmeling on behalf of the Authors (09 Jun 2022) Manuscript

Short summary

Fluid flow through rock occurs in many geological settings on different scales, at different temperature conditions and with different flow velocities. Fluid is either in local thermal equilibrium with the host rock or not. We explore the parameters of porous flow and give scaling laws. These allow us to decide whether porous flows are in thermal equilibrium or not. Applied to magmatic systems, moving melts in channels or dikes moderately to strongly deviate from thermal equilibrium.