Iron Oxide (III) and aluminum oxide (α) were mixed at the molar ratio of 1 to 2, fired for 3 hours under various oxygen partial pressure (P
02); 3.9×10
-7Pa≤P
02≤2.1×10
4Pa at 1300°C, , or 4.0×10
-6Pa≤P
02≤2.1×10
4Pa at 1400°C. The lattice constant of the iron spinel and the valence of iron ions were measured. From the X-ray powder diffraction pattern, the distribution of iron ions was obtained by the PFSR method. The lattice constant was almost constant at low P
02, increased gradually with the increase of P
02, then increased steeply at P
02≈10
-1.5Pa (1300°C), or P
02≈10
0Pa (1400°C), and finally remained unchanged at high P
02. The valence of iron ions showed the similar change. At low P
02, the iron ions were all bivalent, and FeAl
2O
4 was produced. About 80% of the tetrahedral sites and 10% of the octahedral sites were occupied by iron ions, because of the tetrahedral site preference of Fe
2+ ions to Al
3+ ions. With the increase of P
02, a part of Fe
2+ ions was oxidized to Fe
3+ ions, and substituted for Al
3+ ions with a smaller radius, resulting in an increase in the lattice constant. In iron spinel containing Fe
3+ ions, the ratio of the tetrahedral sites occupied by iron ions increased because of their tetrahedral site preference over Fe
2+ ions. In the low P
02 region, the oxidation of the iron ions and the substitution of Al
3+ ions in the tetrahedral sites proceed stepwise with increasing P
02. The steep increase of the lattice constant and the amount of Fe
3+ ions observed at a certain P
02 has been explained as due to the remarkable change in the cation distribution accompanying the promotion of the oxidation of Fe
2+ ions.
View full abstract