Kinetics and mechanism of the thermal gas-phase oxidation of 1,1-dichlorodifluoroethene, CF2CCl2, by molecular oxygen in the presence of trifluoromethylhypofluorite, CF3OF
Abstract
The oxidation of CF2CCl2, initiated thermally by the addition of CF3OF to the alkene, has been investigated between 245.1 and 262.3 K. The initial pressures of gases were in the following ranges: CF3OF 0.7–9.2 Torr;† CF2CCl2, 2.9–40.8 Torr; O2, 5.3–661.9 Torr. Numerous runs were made in the presence of N2 at pressures varying from 44.6 to 700.5 Torr. In two runs 355.7 and 403.7 Torr of CF4 were added. The main product was CF2CIC(O)Cl. [graphic omitted], COF2 and COCl2 were formed in minor amounts. The oxidation is a homogeneous chain reaction, whose rate increases with total pressure. The following mechanism, where E = CF2CCl2, R = CF3CCl2, CF3OCF2CCl2 or CF2ClCCl2, R′= CF3, CF3OCF2 or CF2Cl and M = effective pressure, explains the experimental results: CF3OF + E = R + CF3O (1) CF3O + E = R (2), R + O2+ M = RO2+ M (3, 7) 2RO2= 2RO + O2(4,8), RO = R′C(O)Cl + Cl (5,9) Cl + E = R (6), 2R = recombination products (10) R + CF3OF = RF + CF3O (11), RO2+ E = RO2(E)(12) RO2(E)= RO + [graphic omitted] (13), RO2(E)+ O2+ M = RO2(E)O2+ M (14), 2RO2(E)O2= 2RO2(E)O + O2(15), RO2(E)O = RO + COF2+ COCl2(16), k9=(7 ± 3)× 1013 exp (–39.3 ± 6 kJ mol–1/RT) s–1, k12=(1.9 ± 1)× 108 exp (–19.9 ± 6 kJ mol–1/RT) dm3 mol–1 s–1.