摘要
The effect of Ti4+ ion on the formation of magnetite, which were prepared by solid-state route reaction method, were studied by resistivity, Raman and 57Fe M枚ssbauer spectrometry. Resistivity measured in the range of 10 < T < 300 K for Ti4+ magnetite Feub>3鈭?em>xub>Tiub>xub>Oub>4ub> exhibit first order phase transformations at the Verwey transition Tub>vub> for Feub>3ub>Oub>4ub>, Feub>2.98ub>Tiub>0.02ub>Oub>4ub> and Feub>2.97ub>Tiub>0.03ub>Oub>4ub> at 123 K, 121 K and 118 K, respectively. No first order phase transition was observed for Feub>2.9ub>Tiub>0.1ub>Oub>4ub> and small polaron model retraces the semiconducting resistivity behavior with activation energy of about 72 meV. The changes in Raman spectra as a function of doping show that the changes are gradual for samples with higher Ti doping. The Raman active mode for Feub>2.9ub>Tiub>0.1ub>Oub>4ub> at 鈮?34.4 cm鈭? is shifted as compared to parent Feub>3ub>Oub>4ub> at 鈮?70 cm鈭?, inferring that Mn2+ ions are located mostly on the octahedral sites. 57Fe M枚ssbauer spectroscopy probes the site preference of the substitutions and their effect on the hyperfine magnetic fields confirms that Ti4+ ions are located mostly on the octahedral sites of the Feub>3鈭?em>xub>Tiub>xub>Oub>4ub> spinel structure.