Abstract--Mixtures of magnetite and goethite were formed by the slow oxidation of mixed FeCI2-A1C13 solutions in an alkaline environment at room temperature. The compositions of the products ranged from almost exclusively magnetite in Al-free systems to goethite only at AI/(A1 + Fe) ~ 0.3. The magnetic phase consisted of a partly oxidized (Fe2+/Fe 3+ < 0.5), Al-substituted magnetite. The unit-cell edge length a of the magnetite decreased with increasing A1 (Al = 0-0.37 per formula unit, corresponding to 0-14 mole % A1) and decreasing Fe 2+ in the structure as described by the empirical relationship a(A) = 8.3455 + 0.0693 Fe 2~ -0.0789 A1. A correlation between the experimentally determined a and that calculated from the unit-cell edge lengths of end-member magnetite, maghemite, and hercynite was highly significant (r = .96) although shifted by about 0.01 A. M6ssbauer spectra showed A1 to have entered preferentially the tetrahedral rather than the octahedral sites at low A1 substitutions (<0.15 per formula unit), perhaps because of steric reasons. With increasing A1 substitution the crystal size of magnetite decreased and structural strain increased, indicating that the structure had a limited capability to incorporate Al under these synthesis conditions. The capacity of the goethite structure to tolerate more Al may explain why goethite replaced magnetite at higher A1 concentrations.