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...
Main Authors: | , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-09-01
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Series: | Atmospheric Chemistry and Physics |
Online Access: | https://www.atmos-chem-phys.net/18/13481/2018/acp-18-13481-2018.pdf |
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 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 % of the Cl radicals produced on a high radiant-flux day. In contrast,
on a low radiant-flux day, this drops to 14 %, 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 %) 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 % of the Cl radical budget observed here.</p> |
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ISSN: | 1680-7316 1680-7324 |