Hydrated α-Fe2O3(1 over(1, ̄) 0 2) surface structure: Role of surface preparation

  • Kunaljeet S. Tanwar
  • , Jeffrey G. Catalano
  • , Sarah C. Petitto
  • , Sanjit K. Ghose
  • , Peter J. Eng
  • , Thomas P. Trainor

Research output: Contribution to journalArticlepeer-review

58 Scopus citations

Abstract

The surface structure of α-Fe2 O3 (1 over(1, ̄) 0 2) was studied under two different surface preparation conditions using crystal truncation rod (CTR) diffraction. Wet chemical and mechanical polishing (CMP) at 298 K results in a crystalline surface termination in which the top layer of iron atoms is absent compared to the stoichiometric bulk termination. Annealing in air at 773 K resulted in a transformation of the surface to a structure consistent with hydroxylation of the stoichiometric termination. These results agree with theoretical predictions of Lo et al. [C.S. Lo, K.S. Tanwar, A.M. Chaka, T.P. Trainor, Phys. Rev. B 75 (2007) 075425] and clearly show an ambient pressure surface preparation path leading to a stoichiometric hydroxylated surface, which is apparently a meta-stable configuration at room temperature.

Original languageEnglish
Pages (from-to)L59-L64
JournalSurface Science
Volume601
Issue number12
DOIs
StatePublished - Jun 15 2007

Keywords

  • Crystal truncation rods
  • Hematite (1 over(1, ̄) 0 2)
  • Iron oxide
  • Surface X-ray diffraction
  • Surface annealing
  • Surface preparation
  • Surface structure
  • α-FeO

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