Abstract
We present angle-resolved inverse-photoemission (IPE) spectroscopy data from the nearly perfect (110) surface. Results from two high-symmetry directions of the surface Brillouin zone, Γ¯-X¯ and Γ¯-X¯’, are reported and compared with the results of bulk and surface electronic-structure calculations. Features in the spectra appearing ∼1, 4, 9, and 13 eV above the Fermi level are associated with the primarily Ti-derived 2, 3, 3, and 4 levels. The results are consistent with earlier studies using x-ray-absorption spectroscopy and electron-energy-loss spectroscopy but show some discrepancies in energy positions. All of the spectral features exhibit a small amount of dispersion with respect to . Surface states and resonances identified in the 0–2-eV region are in accordance with previously published calculations [S. Munnix and M. Schmeits, Phys. Rev. B 30, 2202 (1984)]. The absence of surface resonances near 3 eV strongly suggests that the nearly perfect (110) surface is terminated by a bridging oxygen layer.
- Received 2 September 1992
DOI:https://doi.org/10.1103/PhysRevB.47.13722
©1993 American Physical Society