Boiling of Catechol Secondary Organic Aerosol When Heated to Mild Temperatures (36–52 °C) Due to Carbon Dioxide Formation and High Viscosity
Author:
Affiliation:
1. Department of Chemistry, The University of British Columbia, Vancouver V6T 1Z1, British Columbia, Canada
2. Department of Chemistry, University of California−Irvine, Irvine, California 92697, United States
Funder
Canada Foundation for Innovation
Division of Atmospheric and Geospace Sciences
Natural Sciences and Engineering Research Council of Canada
Publisher
American Chemical Society (ACS)
Link
https://pubs.acs.org/doi/pdf/10.1021/acsestair.4c00027
Reference72 articles.
1. Oxygenated Aromatic Compounds are Important Precursors of Secondary Organic Aerosol in Biomass-Burning Emissions
2. Nighttime and daytime dark oxidation chemistry in wildfire plumes: an observation and model analysis of FIREX-AQ aircraft data
3. Emissions of Levoglucosan, Methoxy Phenols, and Organic Acids from Prescribed Burns, Laboratory Combustion of Wildland Fuels, and Residential Wood Combustion
4. Global transformation and fate of SOA: Implications of low-volatility SOA and gas-phase fragmentation reactions
5. Secondary organic aerosol formation in cloud droplets and aqueous particles (aqSOA): a review of laboratory, field and model studies
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