![]() ![]() ![]() Ces mesures ont été réalisées sur une période de plusieurs saisons à Calgary, dans la province de l’Alberta au Canada. Dans le présent article, nous présentons des mesures intermittentes des rapports de mélange du ClNO 2 par spectrométrie de masse à ionisation chimique de l’iode. Le rôle du chlorure de nitryle (ClNO 2) agissant comme réservoir nocturne d’oxyde d’azote et précurseur de chlore atomique dans les zones côtières polluées est bien connu, mais on connaît moins bien son rôle dans les régions continentales. The ubiquity of ClNO 2 implies that the chlorine atom needs to be considered as an oxidant in high-latitude urban environments in winter. The ClNO 2 yield relative to N 2O 5 consumed by heterogeneous reactions was estimated using a time-integrated box model and ranged from 0.5% to 12.1% (10th and 90th percentiles, median 3.4%). The ClNO 2 yield relative to the amount of NO 3 produced from oxidation of NO 2 by O 3 ranged from 0.1% to 4.5% (10th and 90th percentiles, median 1.0%). In the fall, ClNO 2 mixing ratios increased from night to night following the application of salt to roads. Higher ClNO 2 mixing ratios (up to 330 pptv) were observed in the winter and spring months but varied between nights. The lowest ClNO 2 mixing ratios (nocturnal maximum of 30 parts per trillion by volume (pptv)) were observed in the summer, rationalized by losses of the nitrate radical (NO 3) that were more efficient than in the other months. Mixing ratios were highly variable between nights and seasons and depended on the abundances of precursors and meteorological conditions. In this paper, intermittent measurements over the course of several seasons of ClNO 2 mixing ratios by iodide ion chemical ionization mass spectrometry in Calgary, Alberta, Canada, are presented. The role of nitryl chloride (ClNO 2) as a nocturnal nitrogen oxide reservoir species and chlorine atom precursor is well established for polluted coastal areas, but its role at midcontinental locations is less clear. ![]()
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