Orthorhombic In(Fe1-xTix)O3+x/2 (0.50≤×≤0.69) and monoclinic In(Fe1-xTix)O3+x/2 (0.73≤×≤0.75) in the system InFeO3-In2Ti2O7 at 1300°C in air. II. Synthesis and crystal structures

Francisco Brown, Noboru Kimizuka*, Yuichi Michiue

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

10 Scopus citations

Abstract

Two solid solutions, In(Fe1-xTix)O3+x/2 (orthorhombic phase, Cmcm, 0.50≤×≤0.69) and In(Fe1-xTix)O3+x/2 (monoclinic phase, C2/m, 0.73≤×≤0.75) in the pseudobinary system InFeO3-In2Ti2O7 were synthesized at 1300°C in air. Their crystal structures which were determined by powder X-ray diffractometry were closely related to those of the delafossite, (hex.)InFeO3 and the pyrochlore. The crystal structural relationships between InFeO3, In(Fe1-xTix)O3+x/2, and the pyrochlore were discussed in terms of the stacking of the two-dimensional closest packed oxygen layers. The isostructural solid solutions, In(Al1-xTix)O3+x/2, In(Cr1-xTix)O3+x/2, In(Ga1-xTix)O3+x/2, In(Fe1/3Ti1/2Mg1/6)O19/6, and In(Ga0.30Ti0.45Mg0.25)O3.10 were also synthesized and their lattice constants were determined.

Original languageEnglish
Pages (from-to)13-22
Number of pages10
JournalJournal of Solid State Chemistry
Volume157
Issue number1
DOIs
StatePublished - 2001

Keywords

  • Delafossite
  • In(FeTi)O
  • InFeO
  • Polytype
  • Pyrochlore
  • Two-dimensional oxygen closest packing

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