Articles | Volume 17, issue 5
Atmos. Chem. Phys., 17, 3453–3474, 2017
https://doi.org/10.5194/acp-17-3453-2017
Atmos. Chem. Phys., 17, 3453–3474, 2017
https://doi.org/10.5194/acp-17-3453-2017

Research article 10 Mar 2017

Research article | 10 Mar 2017

Formation of highly oxygenated low-volatility products from cresol oxidation

Rebecca H. Schwantes et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Rebecca Schwantes on behalf of the Authors (23 Jan 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (01 Feb 2017) by Yinon Rudich
RR by Anonymous Referee #2 (04 Feb 2017)
RR by Anonymous Referee #1 (15 Feb 2017)
ED: Publish as is (15 Feb 2017) by Yinon Rudich
Download
Short summary
Toluene, one of the principle aromatic compounds present in the atmosphere, is oxidized by OH to produce cresol and other products. Here later-generation low-volatility oxygenated products from cresol oxidation by OH are detected in the gas and particle phases. This work identifies a simple and significant mechanism for toluene secondary organic aerosol formation through the cresol pathway. Likely the phenolic pathway of other aromatic compounds is also important for secondary organic aerosol.
Altmetrics
Final-revised paper
Preprint