C. Atterbury et al., A study of the reactions of trifluoromethyl sulfur pentafluoride, SF5CF3, with several positive ions of atmospheric interest, PHYS CHEM P, 3(11), 2001, pp. 1949-1953
An investigation of the bimolecular reactions of several positive ions of a
tmospheric interest, H3O+, NO+, NO2+, O-2(+), H2O+, N2O+, O+, CO2+, CO+, N and N-2(+), with the greenhouse gas SF5CF3 is reported. The thermal rate c
oefficients and ion product distributions have been determined at 300 K usi
ng a selected ion flow tube. H3O+, NO2+ and NO+ are found to be unreactive.
The reaction with O-2(+) proceeds with a rate coefficient significantly le
ss than the capture value ia chemical routes, in which bonds are broken and
formed. The other reagent ions, H2O+, N2O+, O+, CO2+, CO+, N+ and N-2(+) r
eact with SF5CF3 with reaction rate coefficients close to or at the capture
values. With the exception of the reaction with H2O+, all these efficient
reactions occur by dissociative charge transfer, with CF3+ and SF3+ being t
he dominant product ions. CF3+ forms by direct cleavage of the S-C bond in
SF5CF3+, and SF3+ probably from dissociation of (SF4+)* following intramole
cular rearrangement within the lifetime of (SF5CF3+)*. For H2O+, the observ
ed ion branching ratios suggest that the reaction proceeds ia a chemical pa
thway. The reactions of SF5CF3 with cations will destroy this molecule in t
he upper atmosphere.