Different roles of water in secondary organic aerosol formation from toluene and isoprene

Jia, Long; Xu, YongFu

doi:https://doi.org/10.5194/acp-18-8137-2018

Articles | Volume 18, issue 11

https://doi.org/10.5194/acp-18-8137-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-18-8137-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 11

Research article

|

08 Jun 2018

Research article |

| 08 Jun 2018

Different roles of water in secondary organic aerosol formation from toluene and isoprene

Long Jia and YongFu Xu

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Final revised paper (published on 08 Jun 2018)
Preprint (discussion started on 13 Dec 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'review comments', Anonymous Referee #1, 06 Jan 2018
- AC1: 'reply to reviewer 1', Yongfu Xu, 23 Mar 2018
RC2: 'acp-2017-1064 Reviewer Comments', Anonymous Referee #2, 09 Feb 2018
- AC2: 'reply to reviewer 2', Yongfu Xu, 23 Mar 2018

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Yongfu Xu on behalf of the Authors (29 Mar 2018) Author's response Manuscript

ED: Referee Nomination & Report Request started (12 Apr 2018) by Jason Surratt

RR by Anonymous Referee #1 (22 Apr 2018)

RR by Anonymous Referee #2 (26 Apr 2018)

ED: Publish subject to minor revisions (review by editor) (29 Apr 2018) by Jason Surratt

AR by Yongfu Xu on behalf of the Authors (08 May 2018) Author's response Manuscript

ED: Publish as is (20 May 2018) by Jason Surratt

Short summary

In this work, the opposite effects of relative humidity (RH) on secondary organic aerosol (SOA) formation from toluene and isoprene were observed and have been well explained in terms of various experimental data and model simulations. The increase in SOA from toluene under humid conditions is mainly contributed by aqueous reactions of water-soluble products, whereas SOA formation from isoprene-NO₂ irradiations is controlled by stable Criegee intermediates that are greatly influenced by water.