Abstract
The reduction of the Al2 O3: Fe57 system in a hydrogen atmosphere causes the formation of metallic iron clusters yielding hyperfine-split spectra. On firing in air, these clusters are first converted to Fe2 O3, which subsequently dissolves in the lattice to give Fe3+ at the Al3+ site. Vacuum firing, however, merely tends to stabilize the Fe2+ state in addition to the normal Fe3+ state.