The first UK measurements of nitryl chloride using a chemical ionization mass spectrometer in central London in the summer of 2012, and an investigation of the role of Cl atom oxidation. Issue 11 (1st June 2015)

• Record Type: Journal Article
• Authors: Bannan, Thomas J.; Booth, A. Murray; Bacak, Asan; Muller, Jennifer B. A.; Leather, Kimberley E.; Le Breton, Michael; Jones, Benjamin; Young, Dominique; Coe, Hugh; Allan, James; Visser, Suzanne; Slowik, Jay G.; Furger, Markus; Prévôt, André S. H.; Lee, James; Dunmore, Rachel E.; Hopkins, James R.; Hamilton, Jacqueline F.; Lewis, Alastair C.; Whalley, Lisa K.; Sharp, Thomas; Stone, Daniel; Heard, Dwayne E.; Fleming, Zoë L.; Leigh, Roland; Shallcross, Dudley E.; Percival, Carl J.
• Is Part Of: Journal of geophysical research. Volume 120:Issue 11(2015:Jun.)
• Page Start: 5638
• Page End: 5657
• Publication Date: 2015-06-01
• Subjects: Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2014JD022629
• Languages: English
• ISSNs: 2169-897X

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>The first nitryl chloride (ClNO<sub>2</sub>) measurements in the UK were made during the summer 2012 ClearfLo campaign with a chemical ionization mass spectrometer, utilizing an I<sup>−</sup> ionization scheme. Concentrations of ClNO<sub>2</sub> exceeded detectable limits (11 ppt) every night with a maximum concentration of 724 ppt. A diurnal profile of ClNO<sub>2</sub> peaking between 4 and 5 A.M., decreasing directly after sunrise, was observed. Concentrations of ClNO<sub>2</sub> above the detection limit are generally observed between 8 P.M. and 11 A.M. Different ratios of the production of ClNO<sub>2</sub>:N<sub>2</sub>O<sub>5</sub> were observed throughout with both positive and negative correlations between the two species being reported. The photolysis of ClNO<sub>2</sub> and a box model utilizing the Master Chemical Mechanism modified to include chlorine chemistry was used to calculate Cl atom concentrations. Simultaneous measurements of hydroxyl radicals (OH) using low pressure laser‐induced fluorescence and ozone enabled the relative importance of the oxidation of three groups of measured VOCs (alkanes, alkenes, and alkynes) by OH radicals, Cl atoms, and O<sub>3</sub> to be compared. For the day with the maximum calculated Cl atom concentration, Cl atoms in the early morning were the dominant oxidant for alkanes and, over the entire day, contributed 15%, 3%, and 26% toward the oxidation of alkanes, alkenes, and alkynes, respectively.</p> </abstract>