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Rate of the reaction between oxygen monofluoride and ozone

Colussi, A. J. and Grela, M. A. (1994) Rate of the reaction between oxygen monofluoride and ozone. Chemical Physics Letters, 229 (1-2). pp. 134-138. ISSN 0009-2614. https://resolver.caltech.edu/CaltechAUTHORS:20150623-154804938

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Abstract

The upper limit to k_4 (FO+O_3 → products) ⩽ 4.0× 10^(−18) cm^3/molecule s, derived from a reassessment of the F_2-photosensitized decomposition of O_3, severely restricts the possibility that stratospheric ozone might be depleted in cycles involving F/FO_x radicals. A lower limit to k_3 (FO_2+O_3 → products) ⩾ 5 × 10^(−16) cm^3/molecule s, is also estimated.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/0009-2614(94)01021-8DOIArticle
http://www.sciencedirect.com/science/article/pii/0009261494010218PublisherArticle
ORCID:
AuthorORCID
Colussi, A. J.0000-0002-3400-4101
Additional Information:© 1994 Elsevier. Received 7 July 1994; in final form 17 August 1994.
Issue or Number:1-2
Record Number:CaltechAUTHORS:20150623-154804938
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20150623-154804938
Official Citation:A.J. Colussi, M.A. Grela, Rate of the reaction between oxygen monofluoride and ozone: Implications for the atmospheric role of fluorine, Chemical Physics Letters, Volume 229, Issues 1–2, 21 October 1994, Pages 134-138, ISSN 0009-2614, http://dx.doi.org/10.1016/0009-2614(94)01021-8. (http://www.sciencedirect.com/science/article/pii/0009261494010218)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:58510
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:26 Jun 2015 16:04
Last Modified:03 Oct 2019 08:36

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