The rate coefficients and product yields for the reactions of CF3O- wi
th ClONO2, HNO3, HCl, N2O5, So(2), HI, and H2O were measured at 295 K
and similar to 0.4 Torr using the flowing afterglow technique. The rea
ctions of CF3O- with HO(2)NO2 and H2SO4 were also studied qualitativel
y. CF3O- reacts rapidly with ClONO2, HO2NO2, SO2, and HCl by only fluo
ride transfer and with HNO3, HI, and H2SO4 by both fluoride and proton
transfer. CF3O- also reacts with HI to form IF2- and with N2O5 to pro
duce NO3-. CF3O- undergoes a slow clustering reaction with H2O and is
transformed within water clusters into F-. HF and F-.(HF)(2). CF3O- is
unreactive with CH3NO3, CH3C(O)O2NO2, O-3, NO2, CO2, and O-2. These r
esults demonstrate that CF3O- is an excellent candidate as a reagent i
on for the selective detection of ClONO2, HCl, and HNO3 in the upper t
roposphere and stratosphere with a chemical ionization mass spectromet
er. The observed reaction of CF3O- with H(2)0 within water clusters in
dicates that CF3O- will hydrolyze in aqueous solution to form F-, HF,
and CO2. This provides insight into the mechanism for the heterogeneou
s loss of CF3OH in the atmosphere.