Elsevier

Ceramics International

Volume 11, Issue 3, July–September 1985, Pages 80-90
Ceramics International

Paper
HfO2-based refractory compounds and solid solutions: 2. Kinetics and mechanism of compound formation in the systems HfO2single bondM2O3 (MO)

https://doi.org/10.1016/0272-8842(85)90002-1Get rights and content

Abstract

In a previous communication1 we considered the papers published in the USSR on studies of phase diagrams for the systems hafnia-alkali-earth oxides and hafnia — rare-earth oxides. The purpose of many investigations was the preparation of new refractory compounds and solid solutions which could create the basis of high-refractory materials. In addition to the great analogy between binary systems with hafnia and zirconia, our interest in hafnium-containing compounds was promoted by their higher melting temperatures compared with those of zirconia-based compounds and by several peculiar physico-chemical properties characteristic of hafnia-based compounds and solid solutions. It has been shown1 in the HfO2single bondMO systems, strontium forms the greatest number of compounds: SrHfO3, Sr2HfO4, Sr3Hf2O7 and Sr4Hf3O10; calcium forms two compounds: CaHfO3 and CaHf4O9; barium and magnesium each produce one compound: BaHfO3 and Mg2Hf5O12, respectively. Rare earth oxides with large ionic radii usually form pyrochlore-type (P) compounds of composition Ln2Hf2O7, whereas rare-earth oxides with small ionic radii combine with hafnia to form wide regions of fluorite-like solid solutions. In the region of compositions corresponding to the pyrochlore-type compounds rare-earths with the smallest ionic radii (Sc, Yb) form compounds with rhombohedral structures (R) of the composition M4Hf3O12(M7O12). Together with the latter, compounds M7O11.5 and M7O11 were found for gadolinium and erbium and M9O17 and M7O13 for scandium. Most of these compounds are stable only over a certain temperature range and transform into disordered F-type cubic solid solutions at elevated temperatures. In addition, there exist limited regions of solid solutions based on the monoclinic (M) and tetragonal (T) modifications of HfO2 as well as on various structural modifications (C, B, A, H, X) of rare-earth oxides.

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