Rapid dark aging of biomass burning as an overlooked source of oxidized organic aerosol.


Journal

Proceedings of the National Academy of Sciences of the United States of America
ISSN: 1091-6490
Titre abrégé: Proc Natl Acad Sci U S A
Pays: United States
ID NLM: 7505876

Informations de publication

Date de publication:
29 12 2020
Historique:
pubmed: 16 12 2020
medline: 13 2 2021
entrez: 15 12 2020
Statut: ppublish

Résumé

Oxidized organic aerosol (OOA) is a major component of ambient particulate matter, substantially impacting climate, human health, and ecosystems. OOA is readily produced in the presence of sunlight, and requires days of photooxidation to reach the levels observed in the atmosphere. High concentrations of OOA are thus expected in the summer; however, our current mechanistic understanding fails to explain elevated OOA during wintertime periods of low photochemical activity that coincide with periods of intense biomass burning. As a result, atmospheric models underpredict OOA concentrations by a factor of 3 to 5. Here we show that fresh emissions from biomass burning exposed to NO

Identifiants

pubmed: 33318218
pii: 2010365117
doi: 10.1073/pnas.2010365117
pmc: PMC7776776
doi:

Substances chimiques

Aerosols 0
Air Pollutants 0
Particulate Matter 0
Nitrogen Dioxide S7G510RUBH
Oxygen S88TT14065

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

33028-33033

Informations de copyright

Copyright © 2020 the Author(s). Published by PNAS.

Déclaration de conflit d'intérêts

The authors declare no competing interest.

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Auteurs

John K Kodros (JK)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Dimitrios K Papanastasiou (DK)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Marco Paglione (M)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.
Institute of Atmospheric Sciences and Climate, Italian National Research Council, Bologna 40129, Italy.

Mauro Masiol (M)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Stefania Squizzato (S)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Kalliopi Florou (K)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Ksakousti Skyllakou (K)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Christos Kaltsonoudis (C)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece.

Athanasios Nenes (A)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece; athanasios.nenes@epfl.ch spyros@chemeng.upatras.gr.
School of Architecture, Civil and Environmental Engineering, Swiss Federal Institute of Technology Lausanne, Lausanne 1015, Switzerland.

Spyros N Pandis (SN)

Institute of Chemical Engineering Sciences, Foundation for Research & Technology-Hellas, Patras 26504, Greece; athanasios.nenes@epfl.ch spyros@chemeng.upatras.gr.
Department of Chemical Engineering, University of Patras, Patras 26504, Greece.

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