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Sun, Wei1,2,3; Zhang, Guohua1,2,3; Guo, Ziyong1,2,3; Fu, Yuzhen1,2,3; Peng, Xiaocong1,2,3,4; Yang, Yuxiang1,2,3; Hu, Xiaodong1,2,3; Lin, Juying1,2,3,4; Jiang, Feng5; Jiang, Bin1,2,3; Liao, Yuhong1,2,3; Chen, Duohong6; Chen, Jianmin7; Ou, Jie8; Wang, Xinming1,2,3; Peng, Ping'an1,2,3; Bi, Xinhui1,2,3
Formation of In-Cloud Aqueous-Phase Secondary Organic Matter and Related Characteristic Molecules
Source PublicationJOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
ISSN2169-897X
2024-04-16
Volume129Issue:7Pages:13
DOI10.1029/2023JD040355
Language英语
WOS Research AreaMeteorology & Atmospheric Sciences
AbstractAtmospheric particles are largely represented by secondary organic aerosols (SOAs) produced by either aqueous- or gas-phase reactions. Recently, the contribution of the former to SOA formation has been shown to substantially increase and even reach that of the latter, which necessitates in-depth mechanistic investigations. For a deeper understanding of aqueous-phase SOA generation, we herein studied the production of these aerosols in the dark from glycolaldehyde (GAld) and ammonium sulfate (AS)/amines (methylamine (MAm) and glycine (Gly)). UV-vis spectroscopy showed that reaction mixtures featured two main absorption bands (at 209-230 and 280-330 nm) that were attributed to the pi-pi* transitions of Schiff bases and the n-pi* transitions of oligomers produced in the above reactions, respectively. Further studies revealed that irrespective of reactant concentration and pH, all the investigated reactions were well fitted by first-order kinetics and were accelerated by increasing AS/MAm concentrations and solution pH under acidic conditions. The reaction rate constants (determined from changes of absorption at 300 nm) followed the order of Gly (k(I) = 2.39 x 10(-6) s(-1)) > MAm (k(I) = 1.19 x 10(-6) s(-1)) > AS (k(I) = 8.33 x 10(-7) s(-1)) at identical low AS/amine concentrations and were in the order of MAm (k(I) = 2.5 x 10(-6) s(-1)) > AS (k(I) = 1.39 x 10(-6) s(-1)) at high AS/MAm concentrations. The main reaction pathways corresponded to the aldol self-condensation of GAld and the nucleophilic attack of AS/amines on GAld followed by dehydration, which afforded imines as the major products. The stronger light absorption of (GAld + Gly) mixtures than that of (glyoxal/methylglyoxal + Gly) mixtures was ascribed to the increased amount of imine- and carbonyl group-containing products produced in the former case.
Keywordcloud water aqueous-phase reaction molecular composition secondary organic aerosols FT-ICR MS
WOS IDWOS:001192336400001
Indexed BySCI
Citation statistics
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/77044
Collection有机地球化学国家重点实验室
Corresponding AuthorBi, Xinhui
Affiliation1.Chinese Acad Sci, State Key Lab Organ Geochem, Guangzhou Inst Geochem, Guangzhou, Peoples R China
2.Chinese Acad Sci, Guangzhou Inst Geochem, Guangdong Key Lab Environm Protect & Resources Uti, Guangzhou, Peoples R China
3.Guangdong Hong Kong Macao Joint Lab Environm Pollu, Guangzhou, Peoples R China
4.Univ Chinese Acad Sci, Beijing, Peoples R China
5.Karlsruhe Inst Technol, Inst Meteorol & Climate Res, Eggenstein Leopoldshafen, Germany
6.Guangdong Environm Monitoring Ctr, State Environm Protect Key Lab Reg Air Qual Monito, Guangzhou, Peoples R China
7.Fudan Univ, Dept Environm Sci & Engn, Shanghai Key Lab Atmospher Particle Pollut & Preve, Shanghai, Peoples R China
8.Shaoguan Environm Monitoring Ctr, Shaoguan, Peoples R China
Recommended Citation
GB/T 7714
Sun, Wei,Zhang, Guohua,Guo, Ziyong,et al. Formation of In-Cloud Aqueous-Phase Secondary Organic Matter and Related Characteristic Molecules[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2024,129(7):13.
APA Sun, Wei.,Zhang, Guohua.,Guo, Ziyong.,Fu, Yuzhen.,Peng, Xiaocong.,...&Bi, Xinhui.(2024).Formation of In-Cloud Aqueous-Phase Secondary Organic Matter and Related Characteristic Molecules.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,129(7),13.
MLA Sun, Wei,et al."Formation of In-Cloud Aqueous-Phase Secondary Organic Matter and Related Characteristic Molecules".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 129.7(2024):13.
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