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Chemical nature and sources of fine particles in urban Beijing: Seasonality and formation mechanisms
Gu, Yifang1,2; Huang, Ru Jin1; Li, Yongjie3; Duan, Jing1,2; Chen, Qi4; Hu, Weiwei5; Zheng, Yan4; Lin, Chunshui1; Ni, Haiyan1; Dai, Wenting1; Cao, Junji1; Liu, Quan6; Chen, Yang7; Chen, Chunying8; Ovadnevaite, Jurgita9; Ceburnis, Darius9; O'Dowd, Colin9
2020-07-01
Source PublicationEnvironment International
ISSN0160-4120
Volume140
Abstract

To mitigate air pollution in China, a legislative ‘Air Pollution Prevention and Control Action Plan’ has been implemented by the Chinese government since 2013. There is, however, a lack of investigations for long-term trends in the composition, sources and evolution processes of PM (particulate matter with diameter less than 1 μm) after the implementation. To evaluate the effectiveness of these control measures, we present a year-long real-time measurement of the chemical composition of PM at an urban site in Beijing from November 2014 to November 2015, and the results are compared with previous studies from 2008 to 2013 to gain insights into the variations of the chemical composition and sources of PM in Beijing. Large seasonal differences were observed in the mass concentrations of PM species and general declining trend was observed in the last seven years. Specifically, the annual averages of mass concentrations in 2014–2015 decrease by 16–43% (PM), 23–43% (organic aerosol, OA), 38–68% (sulfate), 26–51% (nitrate), 18–33% (ammonium) and 27–38% (chloride) compared to those from 2008 to 2013. During winter and summer, the seasonal mass concentrations of sulfate and nitrate show more significant declines especially in summer 2008 (79% and 81%) and summer 2011 (76% and 77%). The nitrate-to-sulfate ratio is higher in 2014–2015 (1.5 ± 0.6) than that in 2013 (1.0 ± 0.3), largely due to significant reduction in SO emissions, suggesting that nitrate is becoming more important than sulfate in particulate pollution in Beijing. OA is the dominant PM fraction (>45%) in all seasons and the mass concentrations/contributions of both primary and secondary OA show different seasonality. As for the more oxidized oxygenated OA (MO-OOA) and less oxidized oxygenated OA (LO-OOA), the contributions of MO-OOA are much higher than those of LO-OOA (27–62% vs. 6–26%) in both high-pollution and low-pollution days. Aqueous-phase processes are found to facilitate the formation of MO-OOA while photochemical oxidation formation is a major contributor of LO-OOA in winter, and photochemical oxidation plays a major role in the formation of MO-OOA in summer and fall. The current study provides a comprehensive seasonal comparison of chemical composition and formation of PM in Beijing and a pacesetter in tackling PM pollution for other equally polluted megacities, after implementation of more stringent control measures after 2013.

KeywordFine Particles Haze Pollution Secondary Formation Sources
DOI10.1016/j.envint.2020.105732
URLView the original
Indexed BySCIE
Language英語English
WOS Research AreaEnvironmental Sciences & Ecology
WOS SubjectEnvironmental Sciences
WOS IDWOS:000544883300003
Scopus ID2-s2.0-85083857183
Fulltext Access
Citation statistics
Document TypeJournal article
CollectionDEPARTMENT OF CIVIL AND ENVIRONMENTAL ENGINEERING
Corresponding AuthorHuang, Ru Jin; Chen, Qi
Affiliation1.State Key Laboratory of Loess and Quaternary Geology, Center for Excellence in Quaternary Science and Global Change, Key Laboratory of Aerosol Chemistry & Physics, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, 710061, China
2.University of Chinese Academy of Sciences, Beijing, 100049, China
3.Department of Civil and Environmental Engineering, Faculty of Science and Technology, University of Macau, Taipa, 999078, China
4.State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China
5.State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China
6.Beijing Weather Modification Office, Beijing, 100089, China
7.Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing, 400714, China
8.CAS Key Laboratory for Biomedical Effects of Nanomaterials and Nanosafety & Beijing Key Laboratory of Ambient Particles Health Effects and Prevention Techniques, National Center for Nanoscience and Technology of China, Beijing, 100190, China
9.School of Physics and Centre for Climate and Air Pollution Studies, Ryan Institute, National University of Ireland Galway, Galway, University Road, H91CF50, United Kingdom
Recommended Citation
GB/T 7714
Gu, Yifang,Huang, Ru Jin,Li, Yongjie,et al. Chemical nature and sources of fine particles in urban Beijing: Seasonality and formation mechanisms[J]. Environment International, 2020, 140.
APA Gu, Yifang., Huang, Ru Jin., Li, Yongjie., Duan, Jing., Chen, Qi., Hu, Weiwei., Zheng, Yan., Lin, Chunshui., Ni, Haiyan., Dai, Wenting., Cao, Junji., Liu, Quan., Chen, Yang., Chen, Chunying., Ovadnevaite, Jurgita., Ceburnis, Darius., & O'Dowd, Colin (2020). Chemical nature and sources of fine particles in urban Beijing: Seasonality and formation mechanisms. Environment International, 140.
MLA Gu, Yifang,et al."Chemical nature and sources of fine particles in urban Beijing: Seasonality and formation mechanisms".Environment International 140(2020).
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