Thermal expansion measurements on various oxide compounds crystallizing with the orthorhombic pseudobrookite structure are reported. The unusual expansion anisotropy appears to be a structure-related property. It was observed for all pseudobrookites including the new phases MgTi 1.6Zr 0.4O 5, MgFeNbO 5 and MgFeTaO 5. The highest thermal expansion coincides with the direction of the double chains of strongly distorted (MeO 6)-octahedra. This is in the direction of the c-axis where the shortest 0–0 distances are also found. The smallest, or even “negative”, expansion always occurs in the direction of the a-axis. This is the shortest axis, its length corresponds to the height of the distorted (MeO 6)-octahedra. Isothermal heat treatment and DTA runs proved the instability of Al 2TiO 5, MgFeNbO 5 and, especially, Ga 2TiO 5. Stable compounds like Fe 2TiO 5 and MgTi 2O 5 are formed at much lower temperatures than the unstable compounds Al 2TiO 5 and Ga 2TiO 5 (strongly endothermic reactions at 1360 °–1370 °C). Ga 2TiO 5 decomposes spontaneously and strongly exothermically into the component oxides at about 980 °C. All pseudobrookite compounds are mechanically very weak due to their strong expansion anisotropy.
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