1D Lattice Distortions as the Origin of the (2×2)p4gm Reconstruction in γFe4N(100): A Magnetism-Induced Surface Reconstruction

J. M. Gallego, D. O. Boerma, R. Miranda, and Felix Ynduráin
Phys. Rev. Lett. 95, 136102 – Published 20 September 2005

Abstract

The (100) surface of magnetic γFe4N films epitaxially grown on Cu(100) shows a (2×2)p4gm reconstruction. The atom positions determined experimentally are properly accounted for by first-principles total energy calculations, which further reveal that the (2×2)p4gm reconstruction requires the topmost Fe4N2 plane to be magnetic and effectively decoupled from the rest of the crystal and that it originates from the perpendicular crossing of one-dimensionally dimerized Fe chains.

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  • Received 22 December 2004

DOI:https://doi.org/10.1103/PhysRevLett.95.136102

©2005 American Physical Society

Authors & Affiliations

J. M. Gallego1, D. O. Boerma2, R. Miranda2, and Felix Ynduráin2

  • 1Instituto de Ciencia de Materiales de Madrid-CSIC, Cantoblanco, 28049-Madrid, Spain
  • 2Departamento de Física de la Materia Condensada and Instituto de Ciencia de Materiales Nicolas Cabrera, Universidad Autónoma de Madrid, Cantoblanco, 28049-Madrid, Spain

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Vol. 95, Iss. 13 — 23 September 2005

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