Cr-substituted Ni-Zn ferrites via oxalate decomposition. Structural, electrical and magnetic properties

被引:0
作者
Gabal, M.A. [1 ]
Al Angari, Y.M. [1 ]
Al-Agel, F.A. [2 ]
机构
[1] Chemistry department, Faculty of Science, King Abdulaziz University, Jeddah
[2] Physics department, Faculty of Science, King Abdulaziz University, Jeddah
关键词
Conductivity; Cr-substitution; ferrite; Hysteresis; NiZn; Susceptibility;
D O I
10.1016/j.jmmm.2015.04.115
中图分类号
学科分类号
摘要
Abstract A series of Cr-substituted Ni-Zn ferrites; Ni0.8Zn0.2CrxFe2-xO4 (x=0.0-1.0) were prepared via oxalate decomposition route to characterize the effect of Cr-substitution on structural, magnetic and electrical properties. The prepared powders were characterized using X-ray diffraction (XRD), Fourier transform infrared (FT-IR) and transmission electron microscopy (TEM). XRD indicated single-phase cubic ferrites. The lattice parameters (aExp) exhibited a gradual decrease with increasing chromium, attributed to the smaller ionic radii of Cr3+ substituent. According to the obtained structural data, an appropriate cation distribution was suggested and fortified through FT-IR spectroscopy besides magnetic and electrical measurements. TEM image showed agglomerated cubic crystals with an average size of about 20 nm. Vibrating sample magnetometer (VSM) measurements indicated minimal hysteresis characteristic for soft magnetic material. The decrease in saturation magnetization (Ms) with Cr-substitution was discussed in view of Neel's two sub-lattice model. The change in the coercivity with Cr-content was discussed in view of estimated cation distribution and magnetization values. The obvious fall in the Curie temperature, estimated from molar susceptibility measurements, with increasing Cr-concentrations was assigned to the gradual replacement of Fe3+ ions on the octahedral sites by paramagnetic Cr3+ ions. ac-conductivity as a function of both frequency and absolute temperature exhibited a semi-conducting behavior. The decrease in conductivity with increasing Cr-content was attributed to the preferential occupation of Cr3+ ions by octahedral sites which replacing Fe3+ ions and limiting Fe2+-Fe3+ conduction. © 2015 Elsevier B.V.
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页码:108 / 115
页数:7
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