Formation of Highly Oxidized Organic Compounds and Secondary Organic Aerosol from α-Thujene Ozonolysis
Author:
Affiliation:
1. Department of Chemistry, University of California Irvine, 1120 Natural Sciences II, Irvine, California 92697-2025, United States
Funder
U.S. Department of Energy
National Science Foundation
Publisher
American Chemical Society (ACS)
Subject
Physical and Theoretical Chemistry
Link
https://pubs.acs.org/doi/pdf/10.1021/acs.jpca.3c02584
Reference58 articles.
1. Evolution of Organic Aerosols in the Atmosphere
2. Stocker, T. F.; Qin, D.; Plattner, M.; Tignor, S. K.; Allen, J.; Boschung, A.; Nauels, Y.; Xia, V.; Midgley, B.; PM Climate Change 2013: The Physical Science Basis, Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, 2013, p 1535.
3. A large source of low-volatility secondary organic aerosol
4. The formation, properties and impact of secondary organic aerosol: current and emerging issues
5. The role of low-volatility organic compounds in initial particle growth in the atmosphere
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