TY - JOUR
T1 - Unprecedented Ambient Sulfur Trioxide (SO3) Detection
T2 - Possible Formation Mechanism and Atmospheric Implications
AU - Yao, Lei
AU - Fan, Xiaolong
AU - Yan, Chao
AU - Kurtén, Theo
AU - Daellenbach, Kaspar R.
AU - Li, Chang
AU - Wang, Yonghong
AU - Guo, Yishuo
AU - Dada, Lubna
AU - Rissanen, Matti P.
AU - Cai, Jing
AU - Tham, Yee Jun
AU - Zha, Qiaozhi
AU - Zhang, Shaojun
AU - Du, Wei
AU - Yu, Miao
AU - Zheng, Feixue
AU - Zhou, Ying
AU - Kontkanen, Jenni
AU - Chan, Tommy
AU - Shen, Jiali
AU - Kujansuu, Joni T.
AU - Kangasluoma, Juha
AU - Jiang, Jingkun
AU - Wang, Lin
AU - Worsnop, Douglas R.
AU - Petäjä, Tuukka
AU - Kerminen, Veli Matti
AU - Liu, Yongchun
AU - Chu, Biwu
AU - He, Hong
AU - Kulmala, Markku
AU - Bianchi, Federico
N1 - Funding Information:
The work is supported by Academy of Finland (Center of Excellence in Atmospheric Sciences, project no. 307331, and PROFI3 funding, 311932), the European Research Council via ATM-GTP (742206) and via CHAPAs (850614) and the EMME-CARE project which has received funding from the European Union’s Horizon 2020 Research and Innovation Programme, under Grant Agreement No. 856612.
Publisher Copyright:
© 2020 American Chemical Society. All rights reserved.
Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/11/10
Y1 - 2020/11/10
N2 - Sulfur trioxide (SO3) is a crucial compound for atmospheric sulfuric acid (H2SO4) formation, acid rain formation, and other atmospheric physicochemical processes. During the daytime, SO3is mainly produced from the photo-oxidation of SO2by OH radicals. However, the sources of SO3during the early morning and night, when OH radicals are scarce, are not fully understood. We report results from two field measurements in urban Beijing during winter and summer 2019, using a nitrate-CI-APi-LTOF (chemical ionization-Atmospheric pressure interface-long-Time-of-flight) mass spectrometer to detect atmospheric SO3and H2SO4. Our results show the level of SO3was higher during the winter than during the summer, with high SO3levels observed especially during the early morning (05:00 to 08:30) and night (18:00 to 05:00 the next day). On the basis of analysis of SO2, NOx, black carbon, traffic flow, and atmospheric ions, we suggest SO3could be formed from the catalytic oxidation of SO2on the surface of traffic-related black carbon. This previously unidentified SO3source results in significant H2SO4formation in the early morning and thus promotes sub-2.5 nm particle formation. These findings will help in understanding urban SO3and formulating policies to mitigate secondary particle formation in Chinese megacities.
AB - Sulfur trioxide (SO3) is a crucial compound for atmospheric sulfuric acid (H2SO4) formation, acid rain formation, and other atmospheric physicochemical processes. During the daytime, SO3is mainly produced from the photo-oxidation of SO2by OH radicals. However, the sources of SO3during the early morning and night, when OH radicals are scarce, are not fully understood. We report results from two field measurements in urban Beijing during winter and summer 2019, using a nitrate-CI-APi-LTOF (chemical ionization-Atmospheric pressure interface-long-Time-of-flight) mass spectrometer to detect atmospheric SO3and H2SO4. Our results show the level of SO3was higher during the winter than during the summer, with high SO3levels observed especially during the early morning (05:00 to 08:30) and night (18:00 to 05:00 the next day). On the basis of analysis of SO2, NOx, black carbon, traffic flow, and atmospheric ions, we suggest SO3could be formed from the catalytic oxidation of SO2on the surface of traffic-related black carbon. This previously unidentified SO3source results in significant H2SO4formation in the early morning and thus promotes sub-2.5 nm particle formation. These findings will help in understanding urban SO3and formulating policies to mitigate secondary particle formation in Chinese megacities.
U2 - 10.1021/acs.estlett.0c00615
DO - 10.1021/acs.estlett.0c00615
M3 - Article
AN - SCOPUS:85093941588
SN - 2328-8930
VL - 7
SP - 809
EP - 818
JO - Environmental Science and Technology Letters
JF - Environmental Science and Technology Letters
IS - 11
ER -