Effect of NaOH Concentration and Adding Sequences on Structural and Magnetic Properties of Ni0.4Co0.6Fe2O4 Nanopowders Prepared Via Co-precipitation Route

被引:0
作者
Feng, Jindi [1 ]
Xiong, Rui [2 ,3 ]
Liu, Yong [2 ,3 ]
机构
[1] Xinyang Univ, Sch Sci & Technol, Xinyang 464000, Peoples R China
[2] Wuhan Univ, Sch Phys, Wuhan 430072, Peoples R China
[3] Wuhan Univ, Minist Educ, Key Lab Acoust & Photon Mat & Devices, Wuhan 430072, Peoples R China
基金
中国国家自然科学基金;
关键词
Co-precipitation route; NaOH concentration; Spinel ferrite; Adding sequences of the reagents; Oxidization of Co2+ ions; Metal-oxygen bond; Super-exchange interaction; Tetrahedral sites; Octahedral sites; Sublattice; Noncollinearity; Magneto-crystalline; Anisotropy; Coercivity; FERRITE; CR;
D O I
10.1007/s10948-017-4439-0
中图分类号
O59 [应用物理学];
学科分类号
摘要
Ni0.4Co0.6Fe2O4 nanopowders were prepared via the co-precipitation route followed by annealing treatment. The structural and magnetic properties of the as-synthesized samples were determined by XRD, FT-IR, TG-DSC, and PPMS measurements, respectively. The XRD patterns indicated a single-phase cubic spinel structure for all the Ni-Co ferrite samples, regardless of adding sequences of the reactants or NaOH concentration. The analysis of the XRD patterns revealed that the enhancement in lattice constant with increasing NaOH concentration is related to the prevention of oxidization of Co2+ ions in the Ni-Co ferrite lattice. The FT-IR spectra indicated that samples prepared in the B process have fewer impurities than those prepared in the A process. The enhancement in saturation magnetization with the increase in sodium hydroxide concentration could be attributed to the strengthening of super-exchange interaction between A and B sublattices, due to replacements of Co3+ ions (magnetic moment of 0 mu (B)) by Co2+ ions (magnetic moment of 3 mu (B)) at B sublattices. The obvious increase in the coercivity field with the increase in concentration of NaOH solutions can be interpreted in terms of enhancement of magneto-crystalline anisotropy that originated from gradual substitutions of Co3+ ions with Co2+ ions at the octahedral sites.
引用
收藏
页码:2079 / 2088
页数:10
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