Articles | Volume 24, issue 11
https://doi.org/10.5194/acp-24-6495-2024
https://doi.org/10.5194/acp-24-6495-2024
Research article
 | 
04 Jun 2024
Research article |  | 04 Jun 2024

Daytime and nighttime aerosol soluble iron formation in clean and slightly polluted moist air in a coastal city in eastern China

Wenshuai Li, Yuxuan Qi, Yingchen Liu, Guanru Wu, Yanjing Zhang, Jinhui Shi, Wenjun Qu, Lifang Sheng, Wencai Wang, Daizhou Zhang, and Yang Zhou

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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 egusphere-2023-2698', Anonymous Referee #1, 03 Jan 2024
  • RC2: 'Comment on egusphere-2023-2698', Anonymous Referee #2, 25 Jan 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Yang Zhou on behalf of the Authors (31 Mar 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (10 Apr 2024) by James Allan
RR by Anonymous Referee #2 (10 Apr 2024)
RR by Anonymous Referee #1 (11 Apr 2024)
ED: Publish subject to technical corrections (15 Apr 2024) by James Allan
AR by Yang Zhou on behalf of the Authors (17 Apr 2024)  Author's response   Manuscript 
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Short summary
Aerosol particles from mainland can transport to oceans and deposit, providing soluble Fe and affecting phytoplankton growth. Thus, we studied the dissolution process of aerosol Fe and found that photochemistry played a key role in promoting Fe dissolution in clean conditions. RH-dependent reactions were more influential in slightly polluted conditions. These results highlight the distinct roles of two weather-related parameters (radiation and RH) in influencing geochemical cycles related to Fe.
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