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Winter ClNO2 formation in the region of fresh anthropogenic emissions: seasonal variability and insights into daytime peaks in northern China

Authors :
Wang Zhe
Chuan Yu
Jian Gao
Jianmin Chen
Hong Li
Chenglong Zhang
Hui Chen
Tao Wang
Pengfei Liu
Yujing Mu
Yee Jun Tham
Xiang Peng
Weihao Wang
Xinfeng Wang
Likun Xue
Men Xia
Source :
Atmospheric Chemistry and Physics. 21:15985-16000
Publication Year :
2021
Publisher :
Copernicus GmbH, 2021.

Abstract

Nitryl chloride (ClNO 2 ) is an important chlorine reservoir in the atmosphere that affects the oxidation of volatile organic compounds (VOCs) and the production of RO x radicals and ozone (O 3 ). This study presents measurements of ClNO 2 and related compounds at urban, polluted rural, and polluted lower tropospheric (mountaintop) sites in the winter of 2017–2018 over the North China Plain (NCP). The nocturnal concentrations of ClNO 2 were lower at the urban and polluted rural sites but higher at the polluted lower tropospheric site. The winter concentrations of ClNO 2 were generally lower than the summer concentrations that were previously observed at these sites, which was due to the lower nitrate radical (NO 3 ) production rate ( P (NO 3) ) and the smaller N 2 O 5 uptake coefficients ( γ (N 2 O 5) ) in winter, despite the higher ratios of dinitrogen pentoxide (N 2 O 5 ) to NO 3 in winter. Significant daytime peaks of ClNO 2 were observed at all the sites during the winter campaigns, with ClNO 2 mixing ratios of up to 1.3 ppbv. Vertical transport of ClNO 2 from the residual layers and prolonged photochemical lifetime of ClNO 2 in winter may explain the elevated daytime concentrations. The daytime-averaged chlorine radical (Cl) production rates ( P (Cl)) from the daytime ClNO 2 were 0.17, 0.11, and 0.12 ppbv h −1 at the polluted rural, urban, and polluted lower tropospheric sites, respectively, which were approximately 3–4 times higher than the campaign-averaged conditions. Box model calculations showed that the Cl atoms liberated during the daytime peaks of ClNO 2 increased the RO x levels by up to 27 %–37 % and increased the daily O 3 productions by up to 13 %–18 %. Our results provide new insights into the ClNO 2 processes in the lower troposphere impacted by fresh and intense anthropogenic emissions and reveal that ClNO 2 can be an important daytime source of Cl radicals under certain conditions in winter.

Details

ISSN :
16807324
Volume :
21
Database :
OpenAIRE
Journal :
Atmospheric Chemistry and Physics
Accession number :
edsair.doi...........0c7bdf546c2496a60fba7c7054419476