China's Refractories

《中国耐火材料》英文版

China's Refractories ›› 2022, Vol. 31 ›› Issue (2): 40-44.DOI: 10.19691/j.cnki.1004-4493.2022.02.008

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Thermodynamics of Phase Equilibria in FeO-TiO2-Al2O3 System

Oksana M. BORYSENKO*(), Sergey M. LOGVINKOV, Galina M. SHABANOVA, Andrii A. IVASHURA, Alla M. KOROHODSKA   

  1. Kharkiv Polytechnic Institute, National Technical University, Kharkiv 61002, Ukraine
  • Online:2022-06-15 Published:2022-07-05
  • Contact: Oksana M. BORYSENKO
  • About author:Oksana M. Borysenko is a docent, and a doctoral candidate of the Department of Ceramics, Refractory Materials, Glass and Enamels Technology of Kharkiv Polytechnic Institute of National Technical University in Ukraine, majored in technical sciences. Her field of scientific interests embraces refractory nonmetal materials, multicomponent system condition diagrams, solid phase exchange reactions and their conjugation, and the self-organization of phases into dissipative structures. She had more than 130 scientific publications.

Abstract:

This scientific paper discusses the information on the structure of the three-component system FeO-TiO2-Al2O3, which is necessary for the creation of heat-resistant oxide materials. The structure of binary systems: FeO-Al2O3, FeO-TiO2, and Al2O3-TiO2 is described, and the data on the FeO-TiO2-Al2O3 system are presented. The thermodynamic data of all compounds of the system are given, on the basis of which the change in the Gibbs free energy in the temperature range of 8 00-1 900 K for twenty-one exchange reactions was calculated. It has been established that the triangulation of the FeO-TiO2-Al2O3 system changes in five temperature ranges: up to 1 408 K (TiO2 exists in the polymorphic modification-anatase), 1 408-1 537 K (TiO2 exists in the polymorphic modification-rutile and pseudobrookite is stable), 1 537-1 630 K (thialite is stable), 1 630-2 076 K (rearrangement cannot occur) and above 2 076 K (the presence of the stoichiometric compound Al4TiO8 is allowed). Two-phase equilibria up to 1 408 K are stable: Al2O3-FeTiO3, FeTiO3-FeAl2O4, and FeAl2O4-Fe2TiO4; in the temperature range of 1 408-1 537 K: FeAl2O4-TiO2, FeAl2O4-FeTi2O5, FeAl2O4-FeTiO3, and FeAl2O4-Fe2TiO4; in the temperature range of 1 537-1 630 K: FeAl2O4-TiO2, FeAl2O4-FeTi2O5, FeAl2O4-FeTiO3, FeAl2O4-Fe2TiO4, and FeAl2O4-Al2TiO5; in the temperature range of 1 630-2 076 K: FeTi2O5-Al2TiO5, Al2TiO5-FeTiO3, FeTiO3-Al2O3, FeTiO3-FeAl2O4, and FeAl2O4-Fe2TiO4; over 2 076 K: FeTi2O5-Al2TiO5, FeTi2O5-Al4TiO8, Al4TiO8-FeTiO3, Al4TiO8-Fe2TiO4, Al4TiO8-FeO, and Al4TiO8-FeAl2O4.

Key words: phase equilibria, change in Gibbs free energy, triangulation, hercynite, ulvospinel, ilmenite, pseudobrookite, thialite