TY - JOUR
T1 - Reactions of CF3O- with atmospheric trace gases
AU - Huey, L. Gregory
AU - Villalta, Peter W.
AU - Dunlea, Edward J.
AU - Hanson, David R.
AU - Howard, Carleton J.
PY - 1996/1/4
Y1 - 1996/1/4
N2 - The rate coefficients and product yields for the reactions of CF3O- with ClONO2, HNO3, HCl, N2O5, SO2, HI, and H2O were measured at 295 K and ~∼.4 Torr using the flowing afterglow technique. The reactions of CF3O- with HO2NO2 and H2SO4 were also studied qualitatively. CF3O- reacts rapidly with ClONO2, HO2NO2, SO2, and HCl by only fluoride 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 produce 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, O3, NO2, CO2, and O2. These results demonstrate that CF3O- is an excellent candidate as a reagent ion for the selective detection of ClONO2, HCl, and HNO3 in the upper troposphere and stratosphere with a chemical ionization mass spectrometer. The observed reaction of CF3O- with H2O within water clusters indicates that CF3O- will hydrolyze in aqueous solution to form F-, HF, and CO2. This provides insight into the mechanism for the heterogeneous loss of CF3OH in the atmosphere.
AB - The rate coefficients and product yields for the reactions of CF3O- with ClONO2, HNO3, HCl, N2O5, SO2, HI, and H2O were measured at 295 K and ~∼.4 Torr using the flowing afterglow technique. The reactions of CF3O- with HO2NO2 and H2SO4 were also studied qualitatively. CF3O- reacts rapidly with ClONO2, HO2NO2, SO2, and HCl by only fluoride 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 produce 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, O3, NO2, CO2, and O2. These results demonstrate that CF3O- is an excellent candidate as a reagent ion for the selective detection of ClONO2, HCl, and HNO3 in the upper troposphere and stratosphere with a chemical ionization mass spectrometer. The observed reaction of CF3O- with H2O within water clusters indicates that CF3O- will hydrolyze in aqueous solution to form F-, HF, and CO2. This provides insight into the mechanism for the heterogeneous loss of CF3OH in the atmosphere.
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U2 - 10.1021/jp951928u
DO - 10.1021/jp951928u
M3 - Article
AN - SCOPUS:0000902368
SN - 0022-3654
VL - 100
SP - 190
EP - 194
JO - Journal of physical chemistry
JF - Journal of physical chemistry
IS - 1
ER -