Spinodal Decomposition in the Mg–Al–Fe–O System

Abstract

A supersaturated spinel solid solution having a nominal compositional ratio of Mg/Al/Fe = 0.5:1.0:1.5 was prepared using a conventional solid-state reaction at 1573 K in air followed by quenching in ice water. The formula of the resulting spinel structure compound (the spinel) was determined to be (Mg 0.50 AlFe 0.26 2+ Fe 1.24 3+ ) 0.97 O 4 based on a Rietveld refinement and thermogravimetry, indicating a cation-deficient spinel structure having mixed valences of Fe. This spinel was found to decompose to γ-Fe 2 O 3 and a modified, Fe-poor spinel structure compound via a spinodal decomposition below 855 K. The spinodal temperature was estimated using the sidebands appearing in X-ray diffraction patterns in addition to the temperature dependence of magnetization values. This spinodal decomposition was accompanied by the oxidation of Fe 2+ to Fe 3+ and produced a unique gridlike microstructure (with a grid width of approximately 25 nm) along with enhancement of the saturated magnetization of the material. A sample cooled to room temperature in a furnace after heating at 1573 K in air had a lamella structure having a width of approximately 0.1 μm and comprised particles with a mixture of γ-Fe 2 O 3 and the Fe-poor spinel compound on their surfaces. Subsequent heating of this same material to 1373 K in air formed ε-Fe 2 O 3 in the particles. The crystallographic relationship between ε-Fe 2 O 3 and the modified spinel structure compound was a ε // [112̅ ] s , b ε // [1̅ 10] s , and c ε // [111] s (where ε and s indicate the ε-Fe 2 O 3 and spinel, respectively).