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Magnetic properties of rare earth ion (Sm~(3+)) added nanocrystalline Mg-Cd ferrites, prepared by oxalate co-precipitation method

机译:草酸盐共沉淀法制备稀土离子(Sm〜(3+))添加纳米晶Mg-Cd铁氧体的磁性能

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摘要

Nanocrystalline ferrite powder having the general formula Mg_(1-x)Cd_xFe_2O_4+5% Sm~(3+) (x=0,0.2, 0.4, 0.6, 0.8 and 1.0) was synthesized by chemical oxalate co-precipitation technique. The synthesized powder was characterized by X-ray, IR and SEM techniques. The XRD analysis confirms cubic spinel phase with orthoferrite secondary phase. The lattice constant increases with increase in Cd~(2+) content (x). It is smaller than that for pure Mg-Cd ferrites. The average crystallite size lies in the range 28.69-32.66 nm. Saturation magnetization and magnetic moment increase with cadmium content up to x = 0.4 and decrease thereafter. This is attributed to the existence of localized canted spin. The decrease in saturation magnetization and magnetic moment beyond x=0.4 is due to the presence of triangular spin arrangement on B-site. Coercivity and remanent magnetization decrease while Y-K angles increase with Cd~(3+) content. The Sm~(3+) addition improves the magnetic properties.
机译:通过化学草酸盐共沉淀技术合成了通式为Mg_(1-x)Cd_xFe_2O_4 + 5%Sm〜(3+)(x = 0,0.2,0.4,0.6,0.8和1.0)的纳米晶铁氧体粉末。通过X射线,IR和SEM技术对合成粉末进行表征。 XRD分析证实立方尖晶石相与正铁氧体第二相。晶格常数随Cd〜(2+)含量(x)的增加而增加。它比纯Mg-Cd铁氧体小。平均微晶尺寸在28.69-32.66nm范围内。饱和磁化强度和磁矩随镉含量的增加而增加,直至x = 0.4,此后减小。这归因于局部倾斜自旋的存在。超过x = 0.4时,饱和磁化强度和磁矩的减小是由于B位置上存在三角形自旋排列。随着Cd〜(3+)含量的增加,矫顽力和剩磁强度降低,而Y-K角增加。 Sm〜(3+)的添加改善了磁性能。

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