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HERO ID
4739692
Reference Type
Journal Article
Title
Self-Catalytic Reaction of SO3 and NH3 to Produce Sulfamic Acid and Its Implication to Atmospheric Particle Formation
Author(s)
Li, H; Zhong, J; Vehkamaki, H; Kurtén, T; Wang, W; Ge, M; Zhang, S; Li, Z; Zhang, X; Francisco, JS; Zeng, XC
Year
2018
Is Peer Reviewed?
Yes
Journal
Journal of the American Chemical Society
ISSN:
0002-7863
EISSN:
1520-5126
Publisher
AMER CHEMICAL SOC
Location
WASHINGTON
Page Numbers
11020-11028
Language
English
PMID
30088767
DOI
10.1021/jacs.8b04928
Web of Science Id
WOS:000444219100017
URL
https://pubs.acs.org/doi/10.1021/jacs.8b04928
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Abstract
Sulfur trioxide (SO3) is one of the most active chemical species in the atmosphere, and its atmospheric fate has profound implications to air quality and human health. The dominant gas-phase loss pathway for SO3 is generally believed to be the reaction with water molecules, resulting in sulfuric acid. The latter is viewed as a critical component in the new particle formation (NPF). Herein, a new and competitive loss pathway for SO3 in the presence of abundant gas-phase ammonia (NH3) species is identified. Specifically, the reaction between SO3 and NH3, which produces sulfamic acid, can be self-catalyzed by the reactant (NH3). In dry and heavily polluted areas with relatively high concentrations of NH3, the effective rate constant for the bimolecular SO3-NH3 reaction can be sufficiently fast through this new loss pathway for SO3 to become competitive with the conventional loss pathway for SO3 with water. Furthermore, this study shows that the final product of the reaction, namely, sulfamic acid, can enhance the fastest possible rate of NPF from sulfuric acid and dimethylamine by about a factor of two. An alternative source of stabilizer for acid-base clustering in the atmosphere is suggested, and this new mechanism for NPF has implication to improved atmospheric modeling in highly polluted regions.
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