Skip to content

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

Research output: Contribution to journalArticle

  • Michael Priestley
  • Michael Le Breton
  • Thomas J. Bannan
  • Stephen D. Worrall
  • Asan Bacak
  • Andrew R.D. Smedley
  • Ernesto Reyes-Villegas
  • Archit Mehra
  • James Allan
  • Ann R. Webb
  • Dudley E. Shallcross
  • Hugh Coe
  • Carl J. Percival
Original languageEnglish
Pages (from-to)13481-13493
Number of pages13
JournalAtmospheric Chemistry and Physics
Volume18
Issue number18
Early online date21 Sep 2018
DOIs
DateAccepted/In press - 28 Aug 2018
DateE-pub ahead of print - 21 Sep 2018
DatePublished (current) - 30 Sep 2018

Abstract

A number of inorganic (nitryl chloride, ClNO2; chlorine, Cl2; 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 Ig reagent ion. ClOVOCs appear to be mostly photochemical in origin, although direct emission from vehicles is also suggested. Peak concentrations of ClNO2, Cl2 and HOCl reach 506, 16 and 9ppt respectively. The concentrations of ClNO2 are comparable to measurements made in London, but measurements of ClOVOCs, Cl2 and HOCl by this method are the first reported in the UK. Maximum HOCl and Cl2 concentrations are found during the day and ClNO2 concentrations remain elevated into the afternoon if photolysis rates are low. Cl2 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 ClNO2, Cl2 and ClOVOCs to the chlorine radical budget suggests that Cl2 can be a greater source of Cl than ClNO2, 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 Cl2 production and loss pathways are inhibited by reduced photolysis rates. This results in ClNO2 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.

Download statistics

No data available

Documents

Documents

  • Full-text PDF (final published version)

    Rights statement: This is the final published version of the article (version of record). It first appeared online via Copernicus at https://www.atmos-chem-phys.net/18/13481/2018/ . Please refer to any applicable terms of use of the publisher.

    Final published version, 919 KB, PDF document

    Licence: CC BY

DOI

View research connections

Related faculties, schools or groups