Production of N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> in summer in urban Beijing, China

<p>The heterogeneous hydrolysis of dinitrogen pentoxide (N<sub>2</sub>O<sub>5</sub>) has a significant impact on both nocturnal particulate nitrate formation and photochemistry on the following day through the photolysis of nitryl chloride (ClNO<sub>2</sub&g...

Full description

Bibliographic Details
Main Authors: W. Zhou, J. Zhao, B. Ouyang, A. Mehra, W. Xu, Y. Wang, T. J. Bannan, S. D. Worrall, M. Priestley, A. Bacak, Q. Chen, C. Xie, Q. Wang, J. Wang, W. Du, Y. Zhang, X. Ge, P. Ye, J. D. Lee, P. Fu, Z. Wang, D. Worsnop, R. Jones, C. J. Percival, H. Coe, Y. Sun
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/11581/2018/acp-18-11581-2018.pdf
Description
Summary:<p>The heterogeneous hydrolysis of dinitrogen pentoxide (N<sub>2</sub>O<sub>5</sub>) has a significant impact on both nocturnal particulate nitrate formation and photochemistry on the following day through the photolysis of nitryl chloride (ClNO<sub>2</sub>), yet these processes in highly polluted urban areas remain poorly understood. Here we present measurements of gas-phase N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> by high-resolution time-of-flight chemical ionization mass spectrometer (ToF-CIMS) during summer in urban Beijing, China as part of the Air Pollution and Human Health (APHH) campaign. N<sub>2</sub>O<sub>5</sub> and ClNO<sub>2</sub> show large day-to-day variations with average (±1<i>σ</i>) mixing ratios of 79.2±157.1 and 174.3±262.0&thinsp;pptv, respectively. High reactivity of N<sub>2</sub>O<sub>5</sub>, with <i>τ</i> (N<sub>2</sub>O<sub>5</sub>)<sup>−1</sup> ranging from 0.20&thinsp; × &thinsp;10<sup>−2</sup> to 1.46&thinsp; × &thinsp;10<sup>−2</sup>&thinsp;s<sup>−1</sup>, suggests active nocturnal chemistry and a large nocturnal nitrate formation potential via N<sub>2</sub>O<sub>5</sub> heterogeneous uptake. The lifetime of N<sub>2</sub>O<sub>5</sub>, <i>τ</i> (N<sub>2</sub>O<sub>5</sub>), decreases rapidly with the increase in aerosol surface area, yet it varies differently as a function of relative humidity with the highest value peaking at  ∼ &thinsp;40&thinsp;%. The N<sub>2</sub>O<sub>5</sub> uptake coefficients estimated from the product formation rates of ClNO<sub>2</sub> and particulate nitrate are in the range of 0.017–0.19, corresponding to direct N<sub>2</sub>O<sub>5</sub> loss rates of 0.00044–0.0034&thinsp;s<sup>−1</sup>. Further analysis indicates that the fast N<sub>2</sub>O<sub>5</sub> loss in the nocturnal boundary layer in urban Beijing is mainly attributed to its indirect loss via NO<sub>3</sub>, for example through the reactions with volatile organic compounds and NO, while the contribution of the heterogeneous uptake of N<sub>2</sub>O<sub>5</sub> is comparably small (7–33&thinsp;%). High ClNO<sub>2</sub> yields ranging from 0.10 to 0.35 were also observed, which might have important implications for air quality by affecting nitrate and ozone formation.</p>
ISSN:1680-7316
1680-7324