Observations of organic and inorganic chlorinated compounds and their contribution to chlorine radical concentrations in an urban environment in northern Europe during the wintertime

<p>A number of inorganic (nitryl chloride, ClNO<sub>2</sub>; chlorine, Cl<sub>2</sub>; and hypochlorous acid, HOCl) and chlorinated, oxygenated volatile organic compounds (ClOVOCs) have been measured in Manchester, UK during October and November 2014 using time-of-fl...

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Bibliographic Details
Main Authors: M. Priestley, M. le Breton, T. J. Bannan, S. D. Worrall, A. Bacak, A. R. D. Smedley, E. Reyes-Villegas, A. Mehra, J. Allan, A. R. Webb, D. E. Shallcross, H. Coe, C. J. Percival
Format: Article
Language:English
Published: Copernicus Publications 2018-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/13481/2018/acp-18-13481-2018.pdf
Description
Summary:<p>A number of inorganic (nitryl chloride, ClNO<sub>2</sub>; chlorine, Cl<sub>2</sub>; and hypochlorous acid, HOCl) and chlorinated, oxygenated volatile organic compounds (ClOVOCs) have been measured in Manchester, UK during October and November 2014 using time-of-flight chemical ionisation mass spectrometry (ToF-CIMS) with the I<sup>−</sup> reagent ion. ClOVOCs appear to be mostly photochemical in origin, although direct emission from vehicles is also suggested. Peak concentrations of ClNO<sub>2</sub>, Cl<sub>2</sub> and HOCl reach 506, 16 and 9&thinsp;ppt respectively. The concentrations of ClNO<sub>2</sub> are comparable to measurements made in London, but measurements of ClOVOCs, Cl<sub>2</sub> and HOCl by this method are the first reported in the UK. Maximum HOCl and Cl<sub>2</sub> concentrations are found during the day and ClNO<sub>2</sub> concentrations remain elevated into the afternoon if photolysis rates are low. Cl<sub>2</sub> exhibits a strong dependency on shortwave radiation, further adding to the growing body of evidence that it is a product of secondary chemistry. However, night-time emission is also observed. The contribution of ClNO<sub>2</sub>, Cl<sub>2</sub> and ClOVOCs to the chlorine radical budget suggests that Cl<sub>2</sub> can be a greater source of Cl than ClNO<sub>2</sub>, contributing 74&thinsp;% of the Cl radicals produced on a high radiant-flux day. In contrast, on a low radiant-flux day, this drops to 14&thinsp;%, as both Cl<sub>2</sub> production and loss pathways are inhibited by reduced photolysis rates. This results in ClNO<sub>2</sub> making up the dominant fraction (83&thinsp;%) on low radiant-flux days, as its concentrations are still high. As most ClOVOCs appear to be formed photochemically, they exhibit a similar dependence on photolysis, contributing 3&thinsp;% of the Cl radical budget observed here.</p>
ISSN:1680-7316
1680-7324