Ma. Mendes et al., OXYGEN-ATOM TRANSFER TO POSITIVE-IONS - A NOVEL REACTION OF OZONE IN THE GAS-PHASE, Journal of the American Chemical Society, 120(31), 1998, pp. 7869-7874
In the gas phase, neutral ozone (O-3) transfers an oxygen atom to seve
ral positive ions, i.e. the radical cations of pyridines (R-Py+.; R =
H, CH3, C2H5, and Cl), pyrimidine (Pi(+).), and alkyl halides (CH3X+.;
X = Cl and I), and the halogen cations (X+; X = Cl, Br, and I). React
ivity changes drastically within the halogen series (Cl+ much less tha
n Br+ less than or equal to I+), whereas no O-transfer occurs to F+. T
he oxide derivatives R-Py+-O ., Pi(+)-O ., CH3X+-O ., and XO+ are form
ed, as demonstrated by pentaquadrupole (QqQqQ) double- and triple-stag
e mass spectrometry. No oxygen atom transfer occurs, however, in ''inv
erse'' reactions, i.e., those of ionized ozone (O-3(+).) with the corr
esponding neutrals; and charge transfer dominates. Ab initio calculati
ons suggest that O-transfer from ozone to ionized pyridine yields ioni
zed pyridine N-oxide via simple nucleophilic addition of ozone as oppo
sed to 1,3-dipolar cycloaddition. Similar nucleophilic addition follow
ed by Oz loss is also the most likely mechanism for O-transfer from oz
one to the ionized alkyl halides and halogen cations. This novel O-tra
nsfer reaction to positive ions, which expands our knowledge of the ri
ch chemistry of ozone, introduces a new pathway for the gas-phase oxid
ation of halogen atoms, pyridines, pyrimidines, alkyl halides, and ana
logues, and consequently for the gas-phase generation of their chemica
lly interesting but difficult to access ionized oxides.