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 T V, the initially flat surface undergoes a rooflike distortion with a periodicity of ∼0.5 μm due to ferroelastic twinning within monoclinic domains of the low-temperature monoclinic structure. The monoclinic c axis orients in the surface plane, along the [001]c directions. At the atomic scale, the charge-ordered (√2×√2)R45 â̂̃ 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 (√2×√2)R45 â̂̃ reconstruction. Although conceptually similar, the charge-ordered phases of the (100) surface and sub-TV bulk of magnetite are unrelated phenomena. © 2013 American Physical Society.
CITATION STYLE
De La Figuera, J., Novotny, Z., Setvin, M., Liu, T., Mao, Z., Chen, G., … Parkinson, G. S. (2013). Real-space imaging of the Verwey transition at the (100) surface of magnetite. Physical Review B - Condensed Matter and Materials Physics, 88(16). https://doi.org/10.1103/PhysRevB.88.161410
Mendeley helps you to discover research relevant for your work.