“…It is suggested that the quadrupole-spit doublets component is due to the inherent randomness in site occupancy of different ions, the presence of cation vacancies and especially a fraction of finer particles in the superparamagnetic range, which results in no proper magnetic interactions to show a magnetic hyperfine splitting. For the particles below the critical size, thermally induced energy fluctuations can overcome the anisotropy energy and change the direction of the magnetization of a particle from one easy axis to another [26]. In Table 1, however, the parameters of two spectra have an ossbauer spectra recorded at room temperature for ZF and AF samples.…”