(Sub)Surface Mobility of Oxygen Vacancies at the TiO2 Anatase (101) Surface

Philipp Scheiber, Martin Fidler, Olga Dulub, Michael Schmid, Ulrike Diebold, Weiyi Hou, Ulrich Aschauer, and Annabella Selloni
Phys. Rev. Lett. 109, 136103 – Published 28 September 2012
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Abstract

Anatase is a metastable polymorph of TiO2. In contrast to the more widely studied TiO2 rutile, O vacancies (VO’s) are not stable at the anatase (101) surface. Low-temperature STM shows that surface VO’s, created by electron bombardment at 105 K, start migrating to subsurface sites at temperatures 200K. After an initial decrease of the VO density, a temperature-dependent dynamic equilibrium is established where VO’s move to subsurface sites and back again, as seen in time-lapse STM images. We estimate that activation energies for subsurface migration lie between 0.6 and 1.2 eV; in comparison, density functional theory calculations predict a barrier of ca. 0.75 eV. The wide scatter of the experimental values might be attributed to inhomogeneously distributed subsurface defects in the reduced sample.

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  • Received 12 July 2012

DOI:https://doi.org/10.1103/PhysRevLett.109.136103

© 2012 American Physical Society

Authors & Affiliations

Philipp Scheiber1, Martin Fidler1, Olga Dulub2, Michael Schmid1, Ulrike Diebold1,2,*, Weiyi Hou3, Ulrich Aschauer3, and Annabella Selloni3

  • 1Institute of Applied Physics, Vienna University of Technology, Wiedner Hauptstrasse 8-10/134, 1040 Vienna, Austria
  • 2Department of Physics, Tulane University, New Orleans, Louisiana 70118, USA
  • 3Department of Chemistry, Princeton University, Frick Laboratory, Princeton New Jersey 08544, USA

  • *diebold@iap.tuwien.ac.at

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Issue

Vol. 109, Iss. 13 — 28 September 2012

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