Winter ClNO<sub>2</sub> formation in the region of fresh anthropogenic emissions: seasonal variability and insights into daytime peaks in northern China
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Published:2021-10-27
Issue:20
Volume:21
Page:15985-16000
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Xia Men, Peng Xiang, Wang WeihaoORCID, Yu Chuan, Wang ZheORCID, Tham Yee JunORCID, Chen JianminORCID, Chen HuiORCID, Mu YujingORCID, Zhang Chenglong, Liu Pengfei, Xue Likun, Wang XinfengORCID, Gao Jian, Li Hong, Wang TaoORCID
Abstract
Abstract. Nitryl chloride (ClNO2) is an important chlorine reservoir in the
atmosphere that affects the oxidation of volatile organic compounds (VOCs)
and the production of ROx radicals and ozone (O3). This study
presents measurements of ClNO2 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
ClNO2 were lower at the urban and polluted rural sites but higher at
the polluted lower tropospheric site. The winter concentrations of
ClNO2 were generally lower than the summer concentrations that were
previously observed at these sites, which was due to the lower nitrate
radical (NO3) production rate (P(NO3)) and the smaller
N2O5 uptake coefficients (γ(N2O5)) in winter,
despite the higher ratios of dinitrogen pentoxide (N2O5) to NO3
in winter. Significant daytime peaks of ClNO2 were observed at all the
sites during the winter campaigns, with ClNO2 mixing ratios of up to
1.3 ppbv. Vertical transport of ClNO2 from the residual layers and
prolonged photochemical lifetime of ClNO2 in winter may explain the
elevated daytime concentrations. The daytime-averaged chlorine radical (Cl)
production rates (P(Cl)) from the daytime ClNO2 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 ClNO2 increased the ROx levels by up to 27 %–37 % and increased the
daily O3 productions by up to 13 %–18 %. Our results provide new
insights into the ClNO2 processes in the lower troposphere impacted by
fresh and intense anthropogenic emissions and reveal that ClNO2 can be
an important daytime source of Cl radicals under certain conditions in
winter.
Funder
National Natural Science Foundation of China Research Grants Council, University Grants Committee National Key Research and Development Program of China Stem Cell and Translational Research
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference80 articles.
1. Achtert, P., Birmili, W., Nowak, A., Wehner, B., Wiedensohler, A., Takegawa,
N., Kondo, Y., Miyazaki, Y., Hu, M., and Zhu, T.: Hygroscopic growth of
tropospheric particle number size distributions over the North China Plain,
J. Geophys. Res.-Atmos., 114, D00G07, https://doi.org/10.1029/2008JD010921, 2009. 2. An, Z., Huang, R.-J., Zhang, R., Tie, X., Li, G., Cao, J., Zhou, W., Shi,
Z., Han, Y., Gu, Z., and Ji, Y.: Severe haze in northern China: A synergy of
anthropogenic emissions and atmospheric processes, P.
Natl. Acad. Sci. USA, 116, 8657–8666, 2019. 3. Apodaca, R. L., Huff, D. M., and Simpson, W. R.: The role of ice in N2O5 heterogeneous hydrolysis at high latitudes, Atmos. Chem. Phys., 8, 7451–7463, https://doi.org/10.5194/acp-8-7451-2008, 2008. 4. Atkinson, R. and Arey, J.: Atmospheric degradation of volatile organic
compounds, Chem. Rev., 103, 4605–4638, 2003. 5. Atkinson, R. and Lloyd, A. C.: Evaluation of kinetic and mechanistic data
for modeling of photochemical smog, J. Phys. Chem,
Ref. Data, 13, 315-444, 1984.
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