How Metallic Fe Controls the Composition of its Native Oxide

Sebastien Couet, Kai Schlage, Karel Saksl, and Ralf Röhlsberger
Phys. Rev. Lett. 101, 056101 – Published 1 August 2008

Abstract

We have studied in situ the oxidation of ultrathin iron layers and monitored the chemical changes induced by subsequent deposition of Fe metal using hard x-ray absorption spectroscopy. The site sensitivity of the technique allows us to quantify the composition of the layer throughout the oxidation or deposition process. It is found that the thin native oxide incorporates a significant fraction of Fe atoms remaining in a metallic configuration even in the saturated state. Subsequent deposition of Fe leads to a complete reduction of the oxide that adopts an FeO-like structure containing Fe2+ sites only.

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  • Received 18 April 2008

DOI:https://doi.org/10.1103/PhysRevLett.101.056101

©2008 American Physical Society

Authors & Affiliations

Sebastien Couet1,*, Kai Schlage1, Karel Saksl2, and Ralf Röhlsberger1

  • 1Deutsches Elektronen Synchrotron (DESY), Notkestraße 85, 22603 Hamburg, Germany
  • 2Institute of Materials Research, Slovak Academy of Sciences, Watsonova 47, 04353 Kosice, Slovak Republic

  • *Author to whom correspondence should be addressed. sebastien.couet@desy.de

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Vol. 101, Iss. 5 — 1 August 2008

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