Daytime SO 2 chemistry on ubiquitous urban surfaces as a source of organic sulfur compounds in ambient air

Author:

Deng Huifan1234ORCID,Lakey Pascale S. J.5ORCID,Wang Yiqun14,Li Pan14ORCID,Xu Jinli14ORCID,Pang Hongwei1,Liu Jiangping1ORCID,Xu Xin6ORCID,Li Xue678ORCID,Wang Xinming123ORCID,Zhang Yuzhong9ORCID,Shiraiwa Manabu5ORCID,Gligorovski Sasho123ORCID

Affiliation:

1. State Key Laboratory of Organic Geochemistry and Guangdong Provincial Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510 640, China.

2. Guangdong-Hong Kong-Macao Joint Laboratory for Environmental Pollution and Control, Guangzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China.

3. Chinese Academy of Science, Center for Excellence in Deep Earth Science, Guangzhou 510640, China.

4. University of Chinese Academy of Sciences, Beijing, China.

5. Department of Chemistry, University of California, Irvine, Irvine, CA 92687-2025, USA.

6. Institute of Mass Spectrometry and Atmospheric Environment, Jinan University, Guangzhou 510632, China.

7. Guangdong Provincial Engineering Research Center for On-line Source Apportionment System of Air Pollution, Guangzhou 510632, China.

8. Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality, Guangzhou 510632, China.

9. Key Laboratory of Coastal Environment and Resources of Zhejiang Province, School of Engineering, Westlake University, Hangzhou 310024, China.

Abstract

The reactions of sulfur dioxide (SO 2 ) with surface-bound compounds on atmospheric aerosols lead to the formation of organic sulfur (OS) compounds, thereby affecting the air quality and climate. Here, we show that the heterogeneous reaction of SO 2 with authentic urban grime under near-ultraviolet sunlight irradiation leads to a large suite of various organic compounds including OS released in the gas phase. Calculations indicate that at the core area of Guangzhou, building surface uptake of SO 2 is 15 times larger than uptake of SO 2 on aerosol surfaces, yielding ~20 ng m −3 of OS that represents an important fraction of the observed OS compounds (60 to 200 ng m −3 ) in ambient aerosols of Chinese megacities. This chemical pathway occurring during daytime can contribute to the observed fraction of OS compounds in aerosols and improve the understanding of haze formation and urban air pollution.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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