Articles | Volume 20, issue 14
https://doi.org/10.5194/acp-20-9101-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/acp-20-9101-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Jul 2020
Research article |
| 31 Jul 2020
| 31 Jul 2020
Contrasting sources and processes of particulate species in haze days with low and high relative humidity in wintertime Beijing
Ru-Jin Huang
CORRESPONDING AUTHOR
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266061, China
Yao He
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Jing Duan
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, 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, 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
Weiwei Hu
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
Chunshui Lin
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Haiyan Ni
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Wenting Dai
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Junji Cao
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
Yunfei Wu
Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
Renjian Zhang
Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
State Key Laboratory of Loess and Quaternary Geology, Center for
Excellence in Quaternary Science and Global Change, and Key Laboratory of
Aerosol Chemistry and Physics, Institute of Earth and Environment, Chinese
Academy of Sciences, Xi'an 710061, China
School of Physics and Centre for Climate and Air Pollution Studies,
Ryan Institute, National University of Ireland Galway, University Road,
Galway H91CF50, Ireland
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
Thorsten Hoffmann
Institute of Inorganic and Analytical Chemistry, Johannes Gutenberg
University of Mainz, Düesbergweg 10–14, 55128 Mainz, Germany
Colin D. 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
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- Aerosol high water contents favor sulfate and secondary organic aerosol formation from fossil fuel combustion emissions X. Huang et al. 10.1038/s41612-023-00504-1
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- Impact of aging on the sources, volatility, and viscosity of organic aerosols in Chinese outflows T. Feng et al. 10.5194/acp-23-611-2023
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- Heterogeneous interactions between SO<sub>2</sub> and organic peroxides in submicron aerosol S. Wang et al. 10.5194/acp-21-6647-2021
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- Staggered-peak production is a mixed blessing in the control of particulate matter pollution Y. Wang et al. 10.1038/s41612-022-00322-x
- Low-molecular-weight carboxylates in urban southwestern China: Source identification and effects on aerosol acidity W. Guo et al. 10.1016/j.apr.2021.101141
- Characteristics of ice-nucleating particles in Beijing during spring: A comparison study of measurements between the suburban and a nearby mountain area Y. Hu et al. 10.1016/j.atmosenv.2022.119451
- The deep blue day is decreasing in China S. Wang et al. 10.1007/s00704-021-03898-1
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- Variations of PM2.5 sources in the context of meteorology and seasonality at an urban street canyon in Southwest Germany J. Song et al. 10.1016/j.atmosenv.2022.119147
- Secondary Formation of Aerosols Under Typical High‐Humidity Conditions in Wintertime Sichuan Basin, China: A Contrast to the North China Plain Y. Wang et al. 10.1029/2021JD034560
- Chemical composition of NR-PM1 in a coastal city of Southeast China: Temporal variations and formation pathways Y. Chen et al. 10.1016/j.atmosenv.2022.119243
- The formation and evolution of secondary organic aerosol during summer in Xi'an: Aqueous phase processing in fog-rain days J. Duan et al. 10.1016/j.scitotenv.2020.144077
- Composition and sources of particulate matter in the Beijing-Tianjin-Hebei region and its surrounding areas during the heating season X. Dao et al. 10.1016/j.chemosphere.2021.132779
- Sources and processes of organic aerosol in non-refractory PM1 and PM2.5 during foggy and haze episodes in an urban environment of the Yangtze River Delta, China S. Li et al. 10.1016/j.envres.2022.113557
- Evidence of haze-driven secondary production of supermicrometer aerosol nitrate and sulfate in size distribution data in South Korea J. Schlosser et al. 10.5194/acp-22-7505-2022
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- Source apportionment of carbonaceous aerosols in diverse atmospheric environments of China by dual-carbon isotope method M. Li et al. 10.1016/j.scitotenv.2021.150654
- Measurement report: Large contribution of biomass burning and aqueous-phase processes to the wintertime secondary organic aerosol formation in Xi'an, Northwest China J. Duan et al. 10.5194/acp-22-10139-2022
- Exploring the driving factors of haze events in Beijing during Chinese New Year holidays in 2020 and 2021 under the influence of COVID-19 pandemic L. Luo et al. 10.1016/j.scitotenv.2022.160172
- Observed coupling between air mass history, secondary growth of nucleation mode particles and aerosol pollution levels in Beijing S. Hakala et al. 10.1039/D1EA00089F
Latest update: 25 Apr 2024
Short summary
We systematically compared the submicron particle (PM1) processes in haze days with low and high relative humidity (RH) in wintertime Beijing. Nitrate had similar daytime growth rates in low-RH and high-RH pollution. OOA had a higher growth rate in low-RH pollution than in high-RH pollution. Sulfate had a decreasing trend in low-RH pollution, while it increased significantly in high-RH pollution. This distinction may be explained by the different processes affected by meteorological conditions.
We systematically compared the submicron particle (PM1) processes in haze days with low and high...
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