The electronic structure
of isolated Cr(VI) sites supported on
silica was reinvestigated using multiple, complementary electronic
spectroscopies applied to transparent xerogel monoliths. The absorption
spectrum exhibits three previously reported peaks, at 22 800,
29 100, and 41 500 cm–1, as well as
a previously unresolved band at ca. 36 900 cm–1. The emission is a long-lived red luminescence with λmax = 13 600 cm–1, emanating from
the lowest excited state. Assignment of the excited states was facilitated
using time-dependent density functional theory (TD-DFT) calculations
performed on cluster models. All of the observed electronic transitions
and their energies are accounted for by dioxoCr(VI) sites. The lowest
energy observed excitation at 22 800 cm–1 populates a singlet excited state, while the emitting state is the
corresponding triplet state, accessed by intersystem crossing from
the singlet state. Spectroscopic bands observed at 29 100,
36 900, and 41 500 cm–1 were assigned,
based on the TD-DFT calculation, to spin-allowed transitions that
are consistent with emission polarization anisotropy measurements.
Small variations in site symmetry at Cr result principally in inhomogeneous
broadening of the spectral bands, as well as a red-edge effect in
the photoemission spectrum. There is no evidence for a significant
contribution from five-coordinate mono-oxoCr(VI) sites.