Determination of the Bond Energies for the Series O2–O2+ through O2–O10+

Abstract
Equilibrium constants for the reactions O2 + O2n+ = O2n+2+, n = 1–8 , have been determined mass spectrometrically. The fraction of the O4+–O12+ ions which dissociate in the spectrometer is computed theoretically. It is found that a signicant fraction of the O10+ and O12+ ions dissociate in this region. The equilibrium constants are corrected for this and other phenomena. Rotational entropies are computed for the theoretical structures of these complexes. Vibrational entropies are used to estimate weak mode vibrational frequencies. By extrapolation of the enthalpy data to 0°K, the bond energies are found to be D0(O2O2+ = 10.53 ± 0.10, D0(O2O4+) = 6.51 ± 0.07, D0(O2O6+) = 2.56−0.06+0.16, D0(O2O8+) = 2.43−0.09+0.06, and D0(O2–O10+) = 2.0−0.6+0.4kcal/mole . The De(O2O2n+) for n = 3–5 obtained by correcting D0(O2O2n+) for zero‐point energy differences are in reasonable agreement with the values computed by a classical electrostatic model. The vibrational entropy of O4+ at 298°K is found to be 9.93 e.u. This is in good agreement with the theoretical value of 10.21 eu obtained from the theoretical (semiempirical SCF MO) potential surface. Various models are used to analyze the equilibrium constant data to determine the model dependence of the derived quantities. The ΔHn°, ΔSn°, and D0(O2O2n+) values are only weakly dependent on the assumed geometry and weak mode vibrational frequency distribution of the O2n+. On the basis of the De(O2O2n+) values for O8+–O12+, it is tentatively concluded that the frequencies for the O6+ base cluster in O8+–O12+ are close to those of free O6+. The experimental data are not accurate enough to prove this hypothesis.

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