Abstract
Effects of the Verwey transition on the (100) surface of magnetite were studied using scanning tunneling microscopy and spin polarized low-energy electron microscopy. On cooling through the transition temperature , the initially flat surface undergoes a rooflike distortion with a periodicity of m due to ferroelastic twinning within monoclinic domains of the low-temperature monoclinic structure. The monoclinic axis orients in the surface plane, along the directions. At the atomic scale, the charge-ordered () reconstruction of the (100) surface is unperturbed by the bulk transition, and is continuous over the twin boundaries. Time resolved low-energy electron microscopy movies reveal the structural transition to be first order at the surface, indicating that the bulk transition is not an extension of the Verwey-like () reconstruction. Although conceptually similar, the charge-ordered phases of the (100) surface and sub- bulk of magnetite are unrelated phenomena.
- Received 26 June 2013
DOI:https://doi.org/10.1103/PhysRevB.88.161410
This article is available under the terms of the Creative Commons Attribution 3.0 License. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI.
Published by the American Physical Society