The Journal of Chemical Physics · 1977 · 116 citations · 27 references
Natural SciencesChemistryAtmospheric ChemistryAtmospheric ScienceSpectroscopyAtmospheric Oxidation ProcessesAtmospheric Trace GasesLaser SpectroscopyOzone ChemistryPhotochemical KineticsPhotochemistryAtmospheric Trace Gas ChemistryChannelsOzone PhotochemistryOzone Reaction KineticsRate ConstantsTemperature DependenceTemperature Dependence Of Resonance AbsorptionTropospheric Ozone Chemistry
Absolute rate constants are reported for the deactivation of O(1D) by five trace atmospheric constituents for the temperature range 200–350 K. O(1D) atoms produced by photolyzing ozone with a frequency quadrupled pulse from a Nd-YAG laser are monitored directly by means of the O(1D) →O(3P) emission at 630 nm. All the gases studied here are thought to deactivate O(1D) primarily through reactive channels. Their rate constants exhibit no detectable temperature dependence. The rate constants are (in units of 10−10 cm3/molecule⋅s) N2O: 1.1,±0.2, H2: 0.99±0.3, HCl: 1.4±0.4, NH3: 2.5±0.5, CH4: 1.4±0.4. The present results and those of our previous studies are compared with rate constants obtained using the time-resolved attenuation of resonance absorption technique.
27
The quenching of metastable O2(1Δg) and O2(1Σg+) molecules
K. H. Becker, W. Groth, U. Schurath · Chemical Physics Letters · 1971 · 166 citations