Surface Magnetism during Oxygen-Aided Fe Homoepitaxy

M. Nývlt, F. Bisio, J. Franta, C. L. Gao, H. Petek, and J. Kirschner
Phys. Rev. Lett. 95, 127201 – Published 14 September 2005

Abstract

Magnetization-induced optical surface second harmonic generation (SHG) in the longitudinal geometry was used to study magnetism on the p(1×1)O/Fe(001) surface during a layer-by-layer Fe growth with surfactant oxygen. Considerable one-monolayer oscillations were observed. Minima of the magnetization-induced contributions to the second order dielectric susceptibility were detected at half-filled monolayers. These contributions were accessed either by measuring a purely magnetic SHG yield, or indirectly from the magnetization dependence of the overall SHG signal, both providing consistent results. The origin of the oscillatory surface magnetism is consistent with the expected oscillating oxygen induced relaxation due to the surface Fe islands.

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  • Received 26 November 2004

DOI:https://doi.org/10.1103/PhysRevLett.95.127201

©2005 American Physical Society

Authors & Affiliations

M. Nývlt1,2,*, F. Bisio1,3, J. Franta1,2, C. L. Gao1, H. Petek4, and J. Kirschner1

  • 1Max-Planck Institut für Mikrostrukturphysik, Weinberg 2, D-06120 Halle (Saale), Germany
  • 2Faculty of Mathematics and Physics, Institute of Physics, Charles University, Ke Karlovu 5, CZ-121 16 Praha 2, Czech Republic
  • 3Unità INFM, Dipartimento di Fisica, Università di Genova, via Dodecaneso 33, I-16146 Genova, Italy
  • 4Department of Physics and Astronomy, University of Pittsburgh, Pittsburgh, Pennsylvania 15260, USA

  • *Electronic address: nyvlt@karlov.mff.cuni.cz

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Vol. 95, Iss. 12 — 16 September 2005

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