Characteristics, Origins, and Atmospheric Processes of Amines in Fine Aerosol Particles in Winter in China

Author:

Liu Tang1,Xu Yu1ORCID,Sun Qi‐Bin2ORCID,Xiao Hong‐Wei1,Zhu Ren‐Guo3ORCID,Li Chen‐Xi1ORCID,Li Zi‐Yue1,Zhang Kai‐Qi1,Sun Cheng‐Xing1,Xiao Hua‐Yun1ORCID

Affiliation:

1. School of Environmental Science and Engineering Shanghai Jiao Tong University Shanghai China

2. School of Atmospheric Sciences Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies Institute of Earth Climate and Environment System Sun Yat‐sen University Zhuhai China

3. Jiangxi Province Key Laboratory of the Causes and Control of Atmospheric Pollution East China University of Technology Nanchang China

Abstract

AbstractAmines affect particle formation, aerosol acidity, nitrogen cycle, and climate change. However, little is known about the temporal and spatial differences in the composition, source, and formation process of amines in fine particulate matter (PM2.5) in different regions of China. Seven amines (amine salts) were investigated in PM2.5 collected in the Yangtze River Delta (YRD, Shanghai and Nanjing), Pearl River Delta (PRD, Guangzhou), northern China (Xi'an and Haerbin), and background (Puding) areas in winter 2017–2018. Methylamine was the dominant amine species at the YRD, northern China, and background sites, while diethylamine dominated at the PRD site; moreover, the mass concentration and fraction of diethylamine were the lowest at the background site. These results could be attributed to changes in sources and atmospheric processes. Further, coal combustion and biomass burning were found to be important contributors of amines in northern cities in winter. The contribution of biomass and coal combustion to amines was weakened in other urban sites. In contrast, the amine abundance at the background site was largely controlled by biogenic sources. Acid‐base chemistry and displacement mechanism were tightly associated with the formation of amine salts at all sites. In particular, the atmospheric degradation of amines by hydroxyl radical (•OH) was significant at the Nanjing, Guangzhou, Xi'an, and Haerbin sites. The insignificant photochemical degradation of amines at the Shanghai and background sites can be explained by differentiated amine sources, meteorological conditions, and •OH levels. Overall, our findings deepen the understanding of the origins and atmospheric processes of amines.

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

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