A pulse radiolysis system was used to study the kinetics of the reaction of CF&FH02 with NOz. By monitoring the rate of the decay of NO\* using its absorption at 400 nm the reaction rate constant was determined to be k= (5.OkO.S) x 10-r' cm3 molecule-' s-'. A long path length Fourier-transform infra
A kinetic study of the CF3CFHO2 + NO reaction and the dissociation of the CF3CFHO radical
โ Scribed by Ashish Bhatnagar; Robert W. Carr
- Publisher
- Elsevier Science
- Year
- 1995
- Tongue
- English
- Weight
- 582 KB
- Volume
- 238
- Category
- Article
- ISSN
- 0009-2614
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โฆ Synopsis
The kinetics of the reaction of CF,CFHO, radicals with NO was studied by flash photolysis-time-resolved mass spectrometry. From the kinetic growth rate of NO: molecular ions the rate coefficient of the reaction CF,CFHO, + NO -+ CF,CFHO + NO, was determined to be k = (1.31 &-0.30) X 10-l' cm3 molecule-' s -I in the pressure range 12-25 Torr at 324 f 1 K. Measurements of the total NO, yield indicated that the CF,CFHO radicals were completely dissociated by C-C bond scission on the 50 ms time scale of the experiments. The results are discussed in the context of atmospheric chemistry of HFC-134a.
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The kinetics of the self-reactions of HO 2 , CF 3 CFHO 2 , and CF 3 O 2 radicals and the cross reactions of HO 2 with FO 2 , HO 2 with CF 3 CFHO 2 , and HO 2 with CF 3 O 2 radicals, were studied by pulse radiolysis combined with time resolved UV absorption spectroscopy at 295 K. The rate constants f
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The reaction of CF, with NO, was studied at 296 2 2 K using two different absolute techniques Absolute rate constants of ( I 6 ? 0.3) X lo-" and ( 2 1-03+07) X lo-" cm3 molecule-' s-' were derived by IR fluorescence and UV absorption spectroscopy, respectively The reaction proceeds via two reaction
A relative rate approach has , been used to measure the reactivity of CF,O radicals towards ozone. Using k(CFaO+NOa)=2,7x IO-" cm' molecule-' s-' as the referencereactioqanupperlimit ofk(CF,O+Os) 63~ 10-'4cmSmolecule-' was determined at 295 K and 700 Torr of O2 diluent. The implications for the atmo