Ferrite ceramics were prepared utilizing solid state reactions between CuO
and Fe3O4 or alpha-Fe2O3. The samples were analyzed with X-ray diffraction,
Fe-57 Mossbauer and FT-IR spectroscopies. For the solid state reaction bet
ween CuO and Fe3O4, the initial atomic ratios of Cu:Fe varied between 1:299
and 1:2. With an increase in the amount of CuO in the initial reaction mix
ture, there was a corresponding increase in cuprospinel (cubic CuFe2O4) in
the final products of the synthesis. For the initial molar ratio of Cu:Fe =
1:2, cuprospinel phase (0.85) and CuFeO2 phase (0.15) were found by XRD, a
s the result of solid state reaction between CuO and Fe3O4. In this sample,
a small amount of CuO was also detected. For the solid state reaction betw
een CuO and alpha-Fe2O3, the initial molar ratio of 1:1 was used. The sampl
es prepared at a maximum temperature of 800 degrees C, contained similar fr
actions of tetragonal and cubic CuFe2O4 phases, and also minor phases of Cu
O and alpha-Fe2O3 as found by XRD. In the samples prepared at between 1000
and 1350 degrees C, the cubic CuFe2O4 phase was found together with small a
mounts of CuFeO2 and CuO. Mossbauer spectra showed hyperfine field distribu
tions and on the basis of these spectra, calculated parameters, the possibl
e presence of Cu+ and Fe2+ ions in the samples was discussed. For the sampl
es prepared at 1350 degrees C the FT-IR spectrum suggested a significant in
crease in Fe2+ inns, whereas the Mossbauer spectrum and calculated paramete
rs were similar to those for the compound Cu0.7Fe2.3O4. (C) 2000 Elsevier S
cience S.A. All rights reserved.