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Reactivity of Calcium-Bearing Minerals Under Simulated Venus Conditions•SO2 is reactive with several common elements e.g. calcium [1-4]

•Knowledge on chemical reactions has implications for the past and current state of Venus

- Venus may have had liquid water on its surface [5], thus hydrous silicates may have formed at that time [6].
- The Venus Emissivity Mapper (on VERITAS and EnVision) will be used to determine bulk composition of the surface by observing transition metal content [8-9]

- Calcium diffuses through basalt to react with CO2 and SO2, changing the bulk composition and decreasing the emissivity from orbit [8]
- Experiments investigating kinetics will be informative for future emissivity data

•Goal:
- Constrain reaction rate between several calcium minerals and SO2
- Determine the effect, if any, crystal lattices may have on these rates
Document ID
20220016370
Acquisition Source
Glenn Research Center
Document Type
Poster
Authors
S.T. Port
(Oak Ridge Associated Universities Oak Ridge, Tennessee, United States)
A. R. Santos
(Wesleyan University Middletown, Connecticut, United States)
D. Lukco
(HX5, LLC)
T. Kremic
(Glenn Research Center Cleveland, Ohio, United States)
G. W. Hunter
(Glenn Research Center Cleveland, Ohio, United States)
Date Acquired
October 31, 2022
Subject Category
Chemistry And Materials (General)
Lunar And Planetary Science And Exploration
Meeting Information
Meeting: 20th Meeting of the Venus Exploration Analysis Group (VEXAG)
Location: Albuquerque, NM
Country: US
Start Date: November 7, 2022
End Date: November 9, 2022
Sponsors: Lunar and Planetary Institute
Funding Number(s)
WBS: 847801.01.02.01.01
Distribution Limits
Public
Copyright
Portions of document may include copyright protected material.
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