A pulse radiolysis technique has been used to measure a rate constant of (6.6f 1.3) x lo-r2 cm3 molecule-' s-i for the association reaction between CF3C(0)02 radicals and NO2 at 295 K and one atmosphere total pressure of SF, diluent. A FAIR/ smog chamber system was used to study the thermal decompos
Atmospheric chemistry of CF3O radicals: reaction with O3
β Scribed by Timothy J. Wallington; James C. Ball
- Publisher
- Elsevier Science
- Year
- 1995
- Tongue
- English
- Weight
- 574 KB
- Volume
- 234
- Category
- Article
- ISSN
- 0009-2614
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β¦ Synopsis
A relative rate technique has been used to study the title reaction over the pressure range 100-700 Torr of air at 296 + 2 K. Four different reference compounds (13CO, CH4, CH2FCI, and CD 4) were used. Using k(CF30 + CH 4) = (2.2 -1-0.2) Γ 10-14 cm 3 molecule-1 s-1 a rate constant of k(CF30 + 03) = (1.5 + 0.5) Γ 10-14 cm 3 molecule-1 s-1 was derived, quoted errors reflect statistical and potential systematic errors. There was no observable effect of diluent pressure over the range 100-700 Torr. As part of the present work the rate constant for reaction of CF30 radicals with CH2FC1 was determined to be (1.2 + 0.2) Γ 10-14 cm 3 molecule-~ s-1. Implications for the atmospheric chemistry of CF30 radicals are discussed.
π SIMILAR VOLUMES
Rate data for the reactions of CFsO radicals with alkenes and aromatic compounds have been determined at 298 K using a relative rate method. The data are analyzed in terms of structure-reactivity relationships, and their importance to the atmospheric chemistry of CFsO discussed.
The reaction of CF3 radicals with Ha0 (D20) has been studied over the range of 533-723 K using the photolysis and the pyrolysis of CFJ as the free radical source. Arrhenius pa- rameters for the reactions where X = H or D, relative to CF:j radical recombination are given by log kHlkf'2 = (5.12 f 0.1
CF 3 O 2 CF 3 was photolyzed at 254 nm in the presence of CO in 760 torr N 2 or air at 296 K in a static reactor. In N 2 , the products CF 3 OC(O)C(O)OCF 3 and CF 3 OC(O)O 2 C(O)OCF 3 were detected by FTIR spectroscopy. In air, the only observed products were CF 2 O and CO 2 and a chain process, ini
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