RESUMEN
The photophysics of selected tungsten iodide clusters was examined with respect to their role as a photosensitizer for the production of singlet oxygen, O2(a1Δg). We examined all-iodo octahedral clusters, [W6I8(I6)]2-, and ligand-substituted octahedral clusters, [W6I8(L6)]2-, in which the ligand, L, occupies the outer apical positions surrounding the cluster core. We also examined a square-pyramidal cluster, [W5I8(I5)]-, in which the tungsten core was presumably more accessible to diffusional encounter with ground state oxygen, O2(X3Σg-). For the compounds examined, we find pronounced cluster-dependent changes in the yield of photosensitized O2(a1Δg) production. In particular, although the iodine-encased octahedral cluster, [W6I8(I6)]2-, is an efficient O2(a1Δg) sensitizer, the pyramidal cluster, [W5I8(I5)]-, does not make O2(a1Δg) at all. The latter provides fundamental insight into the important case where the sensitizer triplet state is nearly degenerate with the O2(X3Σg-)-O2(a1Δg) transition energy at 1 eV. Our data indicate that even with near resonance, energy transfer to form O2(a1Δg) will not occur within the 3sensitizer-O2(X3Σg-) encounter pair if other more efficient channels for energy dissipation are available.
RESUMEN
The effect of 16 liquid solvents on both the spectrum and molar absorption coefficient of the X3Σg- â b1Σg+ transition in molecular oxygen has been examined. The ability to monitor this weak transition using air or oxygen saturated samples at atmospheric pressure was facilitated by the rapid and efficient O2(b1Σg+) â O2(a1Δg) transition, which allowed the use of O2(a1Δg) phosphorescence as a sensitive probe of O2(b1Σg+) production. The results of these O2(a1Δg) phosphorescence experiments are consistent with the results of independent experiments in which the O2(a1Δg) thus produced was "trapped" via a chemical reaction. The data recorded were used to calculate rate constants for the O2(b1Σg+) â O2(X3Σg-) radiative transition, a parameter that is otherwise difficult to directly obtain from such a wide range of solvents using O2(b1Σg+) â O2(X3Σg-) phosphorescence. The data show that the response of the O2(b1Σg+) â O2(X3Σg-) radiative transition to solvent is not the same as that of the O2(b1Σg+) â O2(a1Δg) and O2(a1Δg) â O2(X3Σg-) radiative transitions, both of which have been extensively examined over the years. However, our data are consistent with a theoretical model proposed by Minaev for the effect of solvent on radiative transitions in oxygen and, as such, arguably provide one of the final chapters in describing a system that has challenged the scientific community for years.