Articles | Volume 13, issue 6
https://doi.org/10.5194/se-13-1045-2022
https://doi.org/10.5194/se-13-1045-2022
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

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on se-2021-149', John Rudge, 12 Jan 2022
    • AC1: 'Reply on RC1', Harro Schmeling, 04 Mar 2022
  • RC2: 'Comment on se-2021-149', Cian Wilson, 24 Jan 2022
    • AC2: 'Reply on RC2', Harro Schmeling, 04 Mar 2022
  • EC1: 'Comment on se-2021-149', Juliane Dannberg, 07 Feb 2022

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 
Download
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.