Structures of FeTiO3 (0001) surfaces observed by scanning tunneling microscopy

Citation
Ra. Fellows et al., Structures of FeTiO3 (0001) surfaces observed by scanning tunneling microscopy, AM MINERAL, 84(9), 1999, pp. 1384-1391
Citations number
30
Categorie Soggetti
Earth Sciences
Journal title
AMERICAN MINERALOGIST
ISSN journal
0003004X → ACNP
Volume
84
Issue
9
Year of publication
1999
Pages
1384 - 1391
Database
ISI
SICI code
0003-004X(199909)84:9<1384:SOF(SO>2.0.ZU;2-E
Abstract
Scanning tunneling microscopy (STM) was used to investigate the (0001) sur face structure of a natural single crystal of FeTiO3, following argon-ion s puttering and annealing in O-2. Low energy electron diffraction (LEED) of t he FeTiO3 (0001) surface shows two different diffraction patterns that depe nd on preparation. We examined surfaces with a hexagonal pattern that was i nterpreted as a (1 x 1) bulk termination. Wide-scale STM images of the (1 x 1) bulk termination show two distinct co-existing areas: large atomically rough terraces and small, smoother, atomically resolved areas within. The o bserved single step height of 2.2 +/- 0.3 Angstrom (doubled values are also found) plus data from the surface orientation implies that two termination types are seen on the (0001) surface after initial stages of preparation, and that these are either cation-terminated surface planes (Fe2+ or Ti4+) o r close-packed oxygen terminations. Atomic-resolution STM images of smooth terrace areas show features arranged in a hexagonal array, with a separatio n of 4.8 +/- 0.2. Angstrom. A model is proposed that identifies this termin ation as an unreconstructed (0001) termination of FeTiO3 that exposes half a layer of either Fe2+ or Ti4+ cations over a close-packed O layer, with ea ch feature arising: from a trimer of O atoms capped by a single cation (Fe2 + or Ti4+).