Mössbauer spectra of Fe2Mo1−xTixO4 (0.2≤x≤1.0) spinel oxides were recorded at 295K in their paramagnetic state. The spectra of all the samples show asymmetric quadrupole split pattern and as molybdenum is progressively replaced by titanium the pattern becomes more and more symmetric. The isomer shift and quadrupole splitting values, inversion parameter and the ratio of Fetotal3+/Fetotal2+ have been calculated from a least-square fitting program. Substitution of molybdenum by titanium in Fe2MoO4, reduces the total Fe3+ and the extent of Fe3+ reduction on tetrahedral (A) and octahedral (B) sites are different. The amount of FeA3+ and FeB3+ions in the x=0.4 and x=0.6 ferrite samples are the same, but their ferrimagnetic Curie temperatures are different, and the former has a compensation temperature which is absent in the latter. This is due to the participation of Mo3+ in the magnetic interactions, which is present in Fe2MoO4, along with Mo4+.
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