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  4. Phosphine on Venus Cannot Be Explained by Conventional Processes

Phosphine on Venus Cannot Be Explained by Conventional Processes

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sword-2021-09-27T14:33:49.original.xml (130 B)
Original SWORD entry document
Author(s)
Bains, William
•
Petkowski, Janusz J
•
Seager, Sara
•
Ranjan, Sukrit
•
Sousa-Silva, Clara
•
Rimmer, Paul B
•
Zhan, Zhuchang
•
Greaves, Jane S
•
Richards, Anita MS
Date Issued
October 1, 2021
Journal
Astrobiology
Publisher
Mary Ann Liebert Inc
Version
Final published version
Abstract
The recent candidate detection of ~1 ppb of phosphine in the middle atmosphere of Venus is so unexpected that it requires an exhaustive search for explanations of its origin. Phosphorus-containing species have not been modelled for Venus' atmosphere before and our work represents the first attempt to model phosphorus species in the Venusian atmosphere. We thoroughly explore the potential pathways of formation of phosphine in a Venusian environment, including in the planet's atmosphere, cloud and haze layers, surface, and subsurface. We investigate gas reactions, geochemical reactions, photochemistry, and other non-equilibrium processes. None of these potential phosphine production pathways are sufficient to explain the presence of ppb phosphine levels on Venus. If PH3's presence in Venus' atmosphere is confirmed, it therefore is highly likely to be the result of a process not previously considered plausible for Venusian conditions. The process could be unknown geochemistry, photochemistry, or even aerial microbial life, given that on Earth phosphine is exclusively associated with anthropogenic and biological sources. The detection of phosphine adds to the complexity of chemical processes in the Venusian environment and motivates in situ follow up sampling missions to Venus. Our analysis provides a template for investigation of phosphine as a biosignature on other worlds.
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Massachusetts Institute of Technology. Department of Physics
Massachusetts Institute of Technology. Department of Aeronautics and Astronautics
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
https://hdl.handle.net/1721.1/135598
DOI of Published Version
https://doi.org/10.1089/ast.2020.2352
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