Articles | Volume 24, issue 8
https://doi.org/10.5194/acp-24-4789-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
Impact of HO2∕RO2 ratio on highly oxygenated α-pinene photooxidation products and secondary organic aerosol formation potential
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- Final revised paper (published on 22 Apr 2024)
- Supplement to the final revised paper
- Preprint (discussion started on 26 Oct 2023)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2023-2402', Anonymous Referee #1, 21 Nov 2023
- AC2: 'Reply on RC1', Thomas Mentel, 30 Jan 2024
- AC4: 'Reply on RC1', Thomas Mentel, 30 Jan 2024
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RC2: 'Comment on egusphere-2023-2402', Anonymous Referee #2, 23 Dec 2023
- AC1: 'Reply on RC2', Thomas Mentel, 30 Jan 2024
- AC3: 'Reply on RC2', Thomas Mentel, 30 Jan 2024
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Thomas Mentel on behalf of the Authors (31 Jan 2024)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (08 Feb 2024) by Sergey A. Nizkorodov
AR by Thomas Mentel on behalf of the Authors (23 Feb 2024)
Author's response
Manuscript
Post-review adjustments
AA – Author's adjustment | EA – Editor approval
AA by Thomas Mentel on behalf of the Authors (09 Apr 2024)
Author's adjustment
Manuscript
EA: Adjustments approved (10 Apr 2024) by Sergey A. Nizkorodov
This work describes experiments aimed at understanding how the chemistry of alpha-pinene oxidation changes under different HO2:RO2 conditions. As described in the paper, this is crucial to understand as high precursor concentrations and low concentrations of small RO2 molecules in chamber experiments lead to lower HO2:RO2 than is generally expected in the real atmosphere. While this is speculated to lead to lower SOA yields, this work shows that as well as evidence for the chemistry shifting when RO2 versus HO2 dominate. Additionally the authors show an interesting method for estimating SOA yields from a CIMS measurement of large gas-phase molecules. This work brings attention to a limitation of interpreting many chamber experiments that show dominant RO2-RO2 chemistry to the real atmosphere. Additionally, this work is thorough in describing their results in the context of known alpha-pinene chemistry and is clear about the limitations in their interpretation. I feel this work fits well within the scope of ACP and I recommend publication once a few issues have been addressed.
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