2692 J. Phys. Chem. B, Vol. 105, No. 14, 2001
Soult et al.
between 30000 and 42000 cm-1 that the titanium did not sit in
an octahedral site. While this is a reasonable conclusion, it is
more compellingly deduced from X-ray data.31 The authors
further concluded that the “remarkable” agreement between the
energies of the experimentally determined absorption maximum
and the predicted maximum proves that the titanium is in a
tetrahedral environment in the silicalite lattice.24
David Gormin for his assistance in determining the phospho-
rescence lifetimes. We thank Dr. Ted Zateslo and Dr. Afi Sachi-
Kocher of the National High Magentic Field Laboratory for
assistance with the ICP-MS measurements. We thank Dr. Bruno
Notari for helpful discussions. The work was conducted under
support provided by the National Science Foundation, Division
of Materials Research, under Grant DMR-9623570.
There is a fundamental problem with this argument that can
be addressed with the spectroscopic data reported here. The
optical electronegativity expression predicts the energy of the
LMCT transitions for only two high-symmetry geometries:
tetrahedral and octahedral. However, it cannot be used to exclude
other, lower symmetry coordination environments that could
easily have LMCT transitions at the same energy as the high-
symmetry species. More importantly, it is clear from the
spectroscopy that the primary assertion that no electronic
absorption is observed below 42000 cm-1 for the titanium site
in TS-1 is simply incorrect.24,25 The emission excitation spectra
clearly show that the emitting state of the titanium is excited at
wavelengths between 32000 and 42000 cm-1. The reason that
absorption bands in the diffuse reflectance electronic spectrum
corresponding to these transitions are not observed until higher
concentrations of titanium are reached is due to the weakness
of the transitions (which are strongly nonallowed), coupled with
the inherent insensitivity of diffuse reflectance techniques.32
These results clearly show that electronic spectroscopy does not
support simple tetrahedral coordination of the titanium in
silicalite. Furthermore, it is not possible to infer a structure from
the electronic spectroscopy, though, consistent with X-ray
analysis, a lower symmetry, four-coordinate species may very
well explain the spectra. It also indicates that the observation
of intensity in the diffuse reflection spectrum in the region below
42000 cm-1 may not necessarily be diagnostic of extraframe-
work titania, especially in samples with higher titanium
concentrations where the weak titanium-based transitions be-
come observable. Conversely, the observation of a strong
absorption in that spectral region, especially at lower titanium
concentrations, is unlikely to be from the titanium site and may
be indicative of extraframework titania or other impurities.
Finally, with regard to the resolved vibrational structure, it is
clear that the ∼960 cm-1 vibrational mode in TS-1 is not
accurately described as a Si-O- stretch “perturbed” by the Ti-
(IV), as has been suggested.11,25,33 The fact that it is an active
progression in the emission spectrum indicates that it is strongly
coupled to the electronic manifold of the titanium and is more
correctly viewed as a Ti-O-Si stretch. Notably, recent
vibrational studies of crystalline titanium silicates tend to support
this interpretation.34
References and Notes
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nm for the tetrehedral model compound Ti(OSi(CH3)3)4. This observation
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site in the lattice. We observed no emission from this compound either in
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Conclusion
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The titanium site in TS-1 catalyst materials has a long-lived
phosphorescent excited state with a maximum at 490 nm in the
near-UV. This state is significantly lower in energy than was
previously suggested by diffuse reflectance absorption spec-
troscopy. Emission excitation spectra indicate that there are weak
electronic absorptions throughout the spectral region from
∼23000 to 48000 cm-1. These observations bring into question
long-standing structural arguments for the coordination of
titanium in the silicalite lattice that have been made using
electronic spectroscopy.
(23) Crocker, M.; Herold, R. H. M.; Roosenbrand, B. G.; Kees, A. E.;
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(25) Zecchina, A.; Spoto, G.; Bordiga, S.; Ferrero, A.; Petrini, G.;
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Acknowledgment. We thank Dr. Eric Lochner of the
Materials Research and Technology Center (MARTECH) at
Florida State University for providing X-ray analysis and Dr.