Articles | Volume 22, issue 2
Atmos. Chem. Phys., 22, 1195–1208, 2022
https://doi.org/10.5194/acp-22-1195-2022
Atmos. Chem. Phys., 22, 1195–1208, 2022
https://doi.org/10.5194/acp-22-1195-2022

Research article 24 Jan 2022

Research article | 24 Jan 2022

Comparison of saturation vapor pressures of α-pinene + O3 oxidation products derived from COSMO-RS computations and thermal desorption experiments

Noora Hyttinen et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on acp-2021-775', Anonymous Referee #1, 17 Oct 2021
  • RC2: 'Comment on acp-2021-775', Anonymous Referee #2, 25 Oct 2021
  • AC1: 'Response to referees', Noora Hyttinen, 02 Dec 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Noora Hyttinen on behalf of the Authors (02 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (06 Dec 2021) by Barbara Ervens
AR by Noora Hyttinen on behalf of the Authors (08 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (08 Dec 2021) by Barbara Ervens
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Short summary
Accurate saturation vapor pressure estimates of atmospherically relevant organic compounds are critical for modeling secondary organic aerosol (SOA) formation. We investigated vapor pressures of highly oxygenated SOA constituents using state-of-the-art computational and experimental methods. We found a good agreement between low and extremely low vapor pressures estimated using the two methods, and the smallest molecules detected in our experiment were likely products of thermal decomposition.
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