Materials of composition Fe3-xSnxO4 (x = 0.1 and 0.2) have been prepar
ed. The Sn-119 Mossbauer spectra show a magnetic hyperfine field demon
strating an interaction between Fe3+ ions on the tetrahedral A sites a
nd Sn4+ ions on the octahedral B sites of Fe3O4. Fe-57 Mossbauer spect
roscopy shows the Curie temperatures of the materials to be lower than
those of magnetite and related titanomagnetites, The Fe-57 and Sn-119
Mossbauer spectra also show the exsolution of tin from the tin-doped
magnetite after prolonged treatment at elevated temperatures. (C) 1996
Academic Press, Inc.