Articles | Volume 23, issue 9
https://doi.org/10.5194/acp-23-5419-2023
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License.
Multiple pathways for the formation of secondary organic aerosol in the North China Plain in summer
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- Final revised paper (published on 16 May 2023)
- Supplement to the final revised paper
- Preprint (discussion started on 29 Aug 2022)
- 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 acp-2022-573', Anonymous Referee #1, 01 Oct 2022
- AC1: 'Reply on RC1', Ru-Jin Huang, 11 Feb 2023
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RC2: 'Comment on acp-2022-573', Anonymous Referee #2, 02 Jan 2023
- AC1: 'Reply on RC1', Ru-Jin Huang, 11 Feb 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Ru-Jin Huang on behalf of the Authors (11 Feb 2023)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to minor revisions (review by editor) (06 Mar 2023) by Samara Carbone
AR by Ru-Jin Huang on behalf of the Authors (06 Mar 2023)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (28 Mar 2023) by Samara Carbone
AR by Ru-Jin Huang on behalf of the Authors (04 Apr 2023)
Manuscript
General comments:
The paper titled “Multiple pathways for the formation of secondary organic aerosol in North China Plain in summer” by Gu et al. reported an summer field observation in Handan City, in which four types of SOA were resolved using the PMF method dealing with the OA mass spectra data from a a soot particle long time-of-flight aerosol mass spectrometer. In addition, the variations and evolution processes of so-called SOA factors were discussed and their formation pathway were then deduced. Although a series of similar studies using AMS data had been reported in NCP previously, this study provided a more detail source appointment results in distinguish SOA as freshly (less-oxidized) and aged (more-oxidized) factors, and further directly associated with the formation pathway (photochemistry and aqueous-phase). With this, a better understanding of ambient SOA formation and aging in complex pollution with high oxidation capacity were gained. The manuscript was well written and presented clearly. Therefore I recommend the publication of Gu et al. work after some issues were clarified and revised.
Specific and technical comments: