Crystal Chemistry and Thermal Behavior in the La ( Cr , Ni ) O 3 Perovskite System

Phase relationships and thermal expansion have been investigated in the system by x‐ray diffraction at room and at high temperatures, by differential thermal analysis, thermogravimetry, and dilatometry. Special attention was paid to the thermal decomposition behavior of in air and flowing oxygen. The rhombohedral perovskite decomposes above 825°C both in air and oxygen to plus and above 1196°C in air (1291°C in oxygen) irreversibly to plus . is orthorhombic at room temperature and transforms at 271°C into a rhombohedral high‐temperature phase which persists at least until 1550°C. The system shows complete miscibility both at room and at higher temperature. In orthorhombic , up to 60% of the Cr can be replaced by Ni at room temperature, while samples containing 70 mole percent (m/o) or more are rhombohedral. The orthorhombic‐rhombohedral phase transition temperature of increases with the incorporation of Ni to a maximum value of 346°C at 20–30 m/o content. The transition temperatures then decrease, as observed by dilatometer measurements. The coefficients of thermal expansion of the rhombohedral high‐temperature phases are always higher than those of the orthorhombic low‐temperature phases (around and , respectively).