Articles | Volume 20, issue 6
https://doi.org/10.5194/acp-20-3793-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-3793-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Summertime and wintertime atmospheric processes of secondary aerosol in Beijing
Jing Duan
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
University of Chinese Academy of Sciences, Beijing 100049, China
Ru-Jin Huang
CORRESPONDING AUTHOR
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
Yongjie Li
Department of Civil and Environmental Engineering, Faculty of Science
and Technology, University of Macau, Taipa, Macau 999078, China
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing 100871, China
Yan Zheng
State Key Joint Laboratory of Environmental Simulation and Pollution
Control, College of Environmental Sciences and Engineering, Peking
University, Beijing 100871, China
Yang Chen
Chongqing Institute of Green and Intelligent Technology, Chinese
Academy of Sciences, Chongqing 400714, China
Chunshui Lin
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
Haiyan Ni
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
Meng Wang
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
Jurgita Ovadnevaite
School of Physics and Centre for Climate and Air Pollution Studies,
Ryan Institute, National University of Ireland Galway, University Road,
Galway, H91CF50, Ireland
Darius Ceburnis
School of Physics and Centre for Climate and Air Pollution Studies,
Ryan Institute, National University of Ireland Galway, University Road,
Galway, H91CF50, Ireland
Chunying Chen
CAS Key Laboratory for Biological Effects of Nanomaterials and
Nanosafety, National Centre for Nanoscience and Technology, Beijing 100191,
China
Douglas R. Worsnop
Aerodyne Research, Inc., Billerica, MA, USA
Thorsten Hoffmann
Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg
University Mainz, Duesbergweg 10–14, 55128 Mainz, Germany
Colin O'Dowd
School of Physics and Centre for Climate and Air Pollution Studies,
Ryan Institute, National University of Ireland Galway, University Road,
Galway, H91CF50, Ireland
Junji Cao
State Key Laboratory of Loess and Quaternary Geology, Key
Laboratory of Aerosol Chemistry and Physics, Institute of Earth
Environment, Chinese Academy of Sciences, Xi'an 710061, China
CAS Center for Excellence in Quaternary Science and Global Change,
Chinese Academy of Sciences, Xi'an 710061, China
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Latest update: 06 Dec 2025
Short summary
We characterized secondary aerosol formation in Beijing. Our results showed that relative humidity (RH) and Ox have opposite effects on sulfate and nitrate formation in summer and winter. The wintertime more-oxidized OOA (MO-OOA) showed a good correlation with aerosol liquid water content (ALWC). Meanwhile, the dependence of less-oxidized OOA (LO-OOA) and the mass ratio of LO-OOA to MO-OOA in Ox both degraded when RH > 60 %, suggesting that RH or ALWC may also affect LO-OOA formation.
We characterized secondary aerosol formation in Beijing. Our results showed that relative...
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