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The reaction of gaseous N sub 2 O sub 5 with solid NaCl at 298 K: Estimated lower limit to the reaction probability and its potential role in tropospheric and stratospheric chemistry

Journal Article · · Geophysical Research Letters (American Geophysical Union); (USA)
DOI:https://doi.org/10.1029/90GL02595· OSTI ID:5548923
;  [1]
  1. California State University, Fullerton (USA)
Gaseous N{sub 2}O{sub 5}/air mixtures were flowed over solid NaCl at 298 K and the gaseous product ClNO{sub 2} measured using FTIR. With excess NaCl, one CINO{sub 2} was produced per N{sub 2}O{sub 5} in the initial mixture, and from the contact time between N{sub 2}O{sub 5} and the salt, a lower limit to the fraction of collisions leading to reaction was estimated to be 2.5 {times} 10{sup {minus}3}. This reaction is sufficiently rapid that it may lead to the formation of ppb levels of ClNO{sub 2} overnight in polluted marine urban areas. The ClNO{sub 2} will photolyze at dawn to give chlorine atoms which initiate the photooxidation of organics in a manner analogous to OH. This reaction may also play a role in remote Arctic chemistry if the reaction is significantly faster than our lower limit. This supports the hypothesis of Michelangeli et al. (1990) that the N{sub 2}O{sub 5(g)} + NaCl{sub (s)} reaction may contribute significantly to stratospheric chemistry after the eruption of alkalic volcanoes such as El Chichon.
OSTI ID:
5548923
Journal Information:
Geophysical Research Letters (American Geophysical Union); (USA), Journal Name: Geophysical Research Letters (American Geophysical Union); (USA) Vol. 18:1; ISSN 0094-8276; ISSN GPRLA
Country of Publication:
United States
Language:
English