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https://doi.org/10.5194/egusphere-2024-1966
https://doi.org/10.5194/egusphere-2024-1966
15 Jul 2024
 | 15 Jul 2024

An elucidatory model of oxygen’s partial pressure inside substomatal cavities

Andrew S. Kowalski

Abstract. A parsimonious model based on Dalton’s law reveals substomatal cavities to be dilute in oxygen (O2), despite photosynthetic O2 production. Transpiration elevates the partial pressure of water vapour but counteractively depresses those of dry air’s components – proportionally including O2 – preserving cavity pressurization that is negligible as regards air composition. Suppression of O2 by humidification overwhelms photosynthetic enrichment, reducing the O2 molar fraction inside cool/warm leaves by hundreds/thousands of ppm. This elucidates the mechanisms that realize O2 transport: diffusion cannot account for up-gradient conveyance of O2 from dilute cavities, through stomata to the more aerobic atmosphere. Rather, leaf O2 emissions depend on non-diffusive transport via mass flow in the form of “stomatal jets” forced by cavity pressurization, which is not negligible in the context of driving viscous flow. Jet expulsion overcomes massive inward O2 diffusion to force net O2 emission. At very high leaf temperatures, jets also influence transport of water vapour and carbon dioxide, physically decoupling their exchanges and reducing water-use efficiency, independent of stomatal regulation.

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Journal article(s) based on this preprint

12 Feb 2025
An elucidatory model of oxygen's partial pressure inside substomatal cavities
Andrew S. Kowalski
Biogeosciences, 22, 785–789, https://doi.org/10.5194/bg-22-785-2025,https://doi.org/10.5194/bg-22-785-2025, 2025
Short summary
Andrew S. Kowalski

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1966', Anonymous Referee #1, 08 Sep 2024
    • AC1: 'Reply on RC1', Andrew Kowalski, 13 Sep 2024
  • RC2: 'Comment on egusphere-2024-1966', Anonymous Referee #2, 21 Sep 2024
    • AC2: 'Reply on RC2', Andrew Kowalski, 25 Sep 2024

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1966', Anonymous Referee #1, 08 Sep 2024
    • AC1: 'Reply on RC1', Andrew Kowalski, 13 Sep 2024
  • RC2: 'Comment on egusphere-2024-1966', Anonymous Referee #2, 21 Sep 2024
    • AC2: 'Reply on RC2', Andrew Kowalski, 25 Sep 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (25 Sep 2024) by Paul Stoy
ED: Reconsider after major revisions (25 Sep 2024) by Paul Stoy (Co-editor-in-chief)
AR by Andrew Kowalski on behalf of the Authors (26 Sep 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Sep 2024) by Paul Stoy
RR by Anonymous Referee #2 (15 Oct 2024)
RR by Anonymous Referee #3 (05 Dec 2024)
ED: Publish subject to minor revisions (review by editor) (12 Dec 2024) by Paul Stoy
ED: Publish subject to minor revisions (review by editor) (13 Dec 2024) by Paul Stoy (Co-editor-in-chief)
AR by Andrew Kowalski on behalf of the Authors (20 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Dec 2024) by Paul Stoy
ED: Publish as is (20 Dec 2024) by Paul Stoy (Co-editor-in-chief)
AR by Andrew Kowalski on behalf of the Authors (24 Dec 2024)  Author's response   Manuscript 

Journal article(s) based on this preprint

12 Feb 2025
An elucidatory model of oxygen's partial pressure inside substomatal cavities
Andrew S. Kowalski
Biogeosciences, 22, 785–789, https://doi.org/10.5194/bg-22-785-2025,https://doi.org/10.5194/bg-22-785-2025, 2025
Short summary
Andrew S. Kowalski
Andrew S. Kowalski

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The requested preprint has a corresponding peer-reviewed final revised paper. You are encouraged to refer to the final revised version.

Short summary
The laws of physics show that leaf oxygen is not photosynthetically enriched, but extremely dilute due to the overwhelming effects of humidification. This challenges the prevailing diffusion-only paradigm regarding leaf gas exchanges, requiring non-diffusive transport. Such transport also explains why fluxes of carbon dioxide and water vapour become decoupled at very high temperatures, as has been observed but not explained by plant physiologists.
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