Chemical Pathways of SO2 with Hydrogen Atoms on Interstellar Ice Analogues

Sulfur dioxide (SO2) is a sulfur-containing molecule expected to exist as a solid in the interstellar medium. In this study, we have performed laboratory experiments and computational studies on the surface reactions of solid SO2 with hydrogen atoms on amorphous solid water (ASW) at low temperatures...

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Bibliographic Details
Published in:The Astrophysical journal 2024-12, Vol.976 (2), p.250
Main Authors: Nguyen, Thanh, Oba, Yasuhiro, Sameera, W. M. C., Furuya, Kenji, Watanabe, Naoki
Format: Article
Language:English
Subjects:
Astrochemistry
Chemical reactions
Codeposition
Hydrogen atoms
Hydrogen sulfide
Ice
Ice formation
Interstellar chemistry
Interstellar matter
Interstellar medium
Laboratory experiments
Low temperature
Pre-biotic astrochemistry
Quantum chemistry
Radicals
Reaction products
Substrates
Sulfur
Sulfur dioxide
Surface reactions
Vapor phases
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Summary:Sulfur dioxide (SO2) is a sulfur-containing molecule expected to exist as a solid in the interstellar medium. In this study, we have performed laboratory experiments and computational studies on the surface reactions of solid SO2 with hydrogen atoms on amorphous solid water (ASW) at low temperatures. After 40 minutes of exposure of SO2 deposited on ASW to H atoms, approximately 80% of the solid SO2 was lost from the substrate at 10–40 K, and approximately 50% even at 60 K, without any definite detection of reaction products. Quantum chemical calculations suggest that H atoms preferentially add to the S atom of solid SO2, forming the HSO2 radical. Further reactions of the HSO2 radical with H atoms result in the formation of several S-bearing species, including HS(O)OH, the S(O)OH radical, HO–S–OH, HS–OH, and H2S. In codeposition experiments involving H and SO2, we have confirmed the formation of H2S, HS(O)OH, and/or HO–S–OH. However, the yields of these S-bearing species are insufficient to account for the complete loss of the initial SO2 reactant. These findings suggest that some products are desorbed into the gas phase upon formation. This study indicates that a portion of the SO2 in ice mantles may remain unreacted, avoiding hydrogenation, while the remainder is converted into other species, some of which may be subject to chemical desorption.
ISSN:0004-637X
1538-4357
DOI:10.3847/1538-4357/ad88ec