Published June 2012 | Version v1
Journal article

A neutron diffraction study of oxygen and nitrogen ordering in a kinetically stable orthorhombic iron doped titanium oxynitride

  • 1. Department of Chemistry, Materials Chemistry Research Centre, University College London, 20 Gordon Street, London, WC1H 0AJ (United Kingdom)
  • 2. School of Chemistry, University of Leeds, Leeds, LS2 9JT (United Kingdom)

Description

The synthesis of a polycrystalline powder sample of iron doped orthorhombic titanium oxynitride, Ti2.92Fe0.01O4.02N0.98, on the scale of 0.7 g has been achieved. This was conducted by the unusual route of delamination from a steel substrate of a thin film deposited using atmospheric pressure chemical vapour deposition. The structure of the titanium oxynitride is presented, determined from a combined analysis of X-ray and neutron powder diffraction data. The use of neutron diffraction allows the position of the oxygen and nitrogen ions in the material to be reported unambiguously for the first time. In this study Ti2.92Fe0.01O4.02N0.98 is found to crystallise in the Cmcm space group, iso-structural pseudobrookite, with lattice parameters a=3.81080(6) Å, b=9.6253(2) Å, and c=9.8859(2) Å, and contains partial oxygen–nitrogen ordering. Of the three anion sites in this structure one is exclusively occupied by oxygen, while the remaining two sites are occupied by oxygen and nitrogen in a disordered manner. Testing indicates that this iron doped titanium oxynitride is a metastable phase that decomposes above 700 °C into TiN and TiO2, the thermodynamic products. - Graphical abstract: We report the synthesis of Ti2.92Fe0.01O4.02N0.98 deposited as a thin film using atmospheric pressure chemical vapour deposition onto stainless steel, which is then delaminated to produce a polycrystalline powder sample. This powder sample was used in a neutron diffraction experiment, and analysis of this data has allowed the position of the oxygen and nitrogen ions in the material to be reported unambiguously for the first time. Ti2.92Fe0.01O4.02N0.98 is found to crystallise in the Cmcm space group iso-structural pseudobrookite and contains partial oxygen–nitrogen ordering. Highlights: ► Partial oxygen and nitrogen ordering has been observed using neutron diffraction. ► A large powder sample has been made by removal of a CVD film from a steel substrate. ► Structural details of Ti2.92Fe0.01O4.02N0.98 are reported for the first time.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.jssc.2012.02.034

Additional details

Identifiers

DOI
10.1016/j.jssc.2012.02.034;
PII
S0022-4596(12)00125-9;

Publishing Information

Journal Title
Journal of Solid State Chemistry
Journal Volume
190
Journal Page Range
p. 169-173
ISSN
0022-4596
CODEN
JSSCBI

Optional Information

Copyright
Copyright (c) 2012 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.