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

被引:0
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作者
Fellows, RA
Lennie, AR
Munz, AW
Vaughan, DJ
Thornton, G
机构
[1] Univ Manchester, Dept Earth Sci, Manchester M13 9PL, Lancs, England
[2] Max Planck Gesell, Fritz Haber Inst, Dept Inorgan Chem, D-14195 Berlin, Germany
[3] Univ Manchester, Dept Chem, Manchester M13 9PL, Lancs, England
[4] Univ Manchester, Interdisciplinary Res Ctr Surface Sci, Manchester M13 9PL, Lancs, England
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中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Scanning tunneling microscopy (STM) was used to investigate the (0001) sur face structure of a natural single crystal of FeTiO3, following argon-ion sputtering and annealing in O-2. Low energy electron diffraction (LEED) of the FeTiO3 (0001) surface shows two different diffraction patterns that depend on preparation. We examined surfaces with a hexagonal pattern that was interpreted 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 observed 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+) or close-packed oxygen terminations. Atomic-resolution STM images of smooth terrace areas show features arranged in a hexagonal array, with a separation of 4.8 +/- 0.2. Angstrom. A model is proposed that identifies this termination 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 each feature arising: from a trimer of O atoms capped by a single cation (Fe2+ or Ti4+).
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页码:1384 / 1391
页数:8
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