Published October 21, 1994
| public
Journal Article
Rate of the reaction between oxygen monofluoride and ozone
- Creators
-
Colussi, A. J.
- Grela, M. A.
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.
Additional Information
© 1994 Elsevier. Received 7 July 1994; in final form 17 August 1994.Additional details
- Eprint ID
- 58510
- Resolver ID
- CaltechAUTHORS:20150623-154804938
- Created
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2015-06-26Created from EPrint's datestamp field
- Updated
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2021-11-10Created from EPrint's last_modified field