Energy partitioning in the reaction O(1D) + H2O → OH + OH.
- 1 July 1981
- journal article
- Published by Elsevier in Chemical Physics Letters
- Vol. 81 (2) , 218-222
- https://doi.org/10.1016/0009-2614(81)80239-4
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Ozone photolysis: determination of the O(3P) quantum yield at 266 nmChemical Physics Letters, 1980
- Inverted and anti-inverted populations of a doublets of chemically produced OHChemical Physics Letters, 1980
- Atmospheric OH production—The O(¹D) + H2O reaction rateGeophysical Research Letters, 1979
- Photofragment spectroscopy of ozone in the uv region 270–310 nm and at 600 nmThe Journal of Chemical Physics, 1978
- Temperature dependence of O(1D) rate constants for reactions with N2O, H2, CH4, HCl, and NH3The Journal of Chemical Physics, 1977
- Absolute rate constant determinations for the deactivation of O(1D) by time resolved decay of O(1D) →O(3P) emissionThe Journal of Chemical Physics, 1976
- Excited State Chemistry in the StratosphereCanadian Journal of Chemistry, 1974
- The Ultraviolet Flash Photolysis of Ozone and the Reaction of O(1D) with H2OCanadian Journal of Chemistry, 1972
- The reaction of OH with NO2 and the deactivation of O(1D) by COInternational Journal of Chemical Kinetics, 1972
- The ultraviolet bands of OH Fundamental dataJournal of Quantitative Spectroscopy and Radiative Transfer, 1962