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Temperature dependence of magnetization, anisotropy and hyperfine fields of NiFe

机译:NiFe的磁化强度,各向异性和超精细场的温度依赖性

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Nickel ferrite (NiFeO), an inverse spinel in which the tetrahedral (A) sites are occupied by Fe ions and the octahedral (B) sites are occupied by Fe and Ni ions, can be represented as Fe Ni Fe O [1-3]. The cation distribution and the resulting magnetic properties are reported to be quite interesting in rare-earth doped nickel ferrite due to the absence of center of symmetry [2, 3]. Kamala Bharathi et al. have reported that, substitution of Fe by Dy ion in NiFeO causes development of magnetocapacitance, leads to ferroelectricity and affects several other properties [3]. These materials play an important role in applications (spintronic memory cell, high frequency devices etc) [4]. There are no reports on thermal behavior of magnetic anisotropy in the rare earth substituted Ni ferrites. Understanding these behaviors will be useful in novel applications such as heat-assisted magnetic recording [4, 5]. In the present work, the temperature dependence of magnetic anisotropy and hyperfine fields of NiFeYbO (x = 0, 0.05, 0.075) are reported. All the samples were prepared by solid state reaction. The materials are found to have formed in inverse spinel structure, from the powder XRD patterns. Rietveld refinement carried out on the XRD patterns revealed that Yb ions occupy the B site and the lattice is found to be expanded with the introduction of Yb. The lattice constants are 8.3415(1) Å (reported value is 8.34 Å [1]), 8.3436(0) Å and 8.3463(5) Å for x = 0, 0.05 and 0.075 compounds respectively. Magnetization was measured at 5 K, 100 K, 200 K, and 300 K and the magnetization was observed to decrease with x. This is attributed to substitution of Fe by Yb in the B-site. The saturation magnetization values, at all the measured temperatures obtained through Honda plots are given in Table 1. The moments calculated using Hund's rule (assuming that Yb and Fe moments are parallel) are 2.82 μ/f.u., 2.76 μ/f.u. and 2.71 μ/f.u. for x = 0, 0.05 and 0.075 compounds respectively. The experimental values are less in comparison with the calculated moments. In NiFeO, this difference is in accordance with the reported literature [1-3]. At each temperature, M-H data were fitted to the law of approach to saturation (LAS) [1, 6] and K1(T), the first order magnetocrystalline anisotropy constant at a temperature T, was obtained from LAS. At any given temperature, the observed increase in K1 of x = 0.05 and 0.075 compared with x = 0, is explained on the basis of single-ion model i.e. localized divalent ions in the octahedral site. The temperature dependence of K1 of cubic systems was investigated by plotting ln K1(T) vs ln M(T). The slopes of the straight line obtained are 7.5, 12.5 and 11.44 for x = 0, 0.05 and 0.075 respectively. This can be compared with the value of 10 proposed for magnetic anisotropy in cubic systems [1, 6]. The deviation of the exponent is explained on the extent of localization of the divalent ion.
机译:铁酸镍(NiFeO)是一种反尖晶石,其中四面体(A)位被Fe离子占据,而八面体(B)位被Fe和Ni离子占据,可以表示为Fe Ni Fe O [1-3] 。据报道,由于缺乏对称中心,在稀土掺杂的镍铁氧体中,阳离子分布和由此产生的磁性能非常有趣[2,3]。卡马拉·巴拉特(Kamala Bharathi)等。据报道,NiFeO中的Dy离子取代Fe会引起磁电容的发展,导致铁电性并影响其他一些性能[3]。这些材料在应用中(自旋电子存储单元,高频设备等)起着重要作用[4]。没有关于稀土取代的镍铁氧体中磁各向异性的热行为的报道。了解这些行为将在诸如热辅助磁记录之类的新型应用中很有用[4,5]。在本工作中,报道了NiFeYbO的磁各向异性和超精细场(x = 0、0.05、0.075)的温度依赖性。所有样品均通过固相反应制备。由粉末XRD图样发现材料已形成反尖晶石结构。在XRD图谱上进行的Rietveld精炼显示,Yb离子占据了B位,并且发现随着Yb的引入,晶格得以扩展。对于x = 0、0.05和0.075的化合物,晶格常数分别为8.3415(1)Å(报告值为8.34Å[1]),8.3436(0)Å和8.3463(5)Å。在5 K,100 K,200 K和300 K下测量磁化强度,观察到磁化强度随x减小。这归因于在B位中Yb取代了Fe。在表1中给出了通过本田图获得的所有测得温度下的饱和磁化强度值。使用洪德法则(假设Yb和Fe的力矩平行)计算的力矩为2.82μ/ f.u.,2.76μ/ f.u。和2.71μ/ f.u。 x分别为0、0.05和0.075。与计算的力矩相比,实验值要小。在NiFeO中,这种差异与已报道的文献一致[1-3]。在每个温度下,M-H数据均符合饱和逼近定律(LAS)[1,6]和K1(T),从LAS获得温度T下的一阶磁晶各向异性常数。在任何给定温度下,根据单离子模型(即八面体位点中的局部二价离子)解释了与x = 0相比x = 0.05和0.075时K1的增加。通过绘制ln K1(T)对ln M(T)来研究立方系统K1的温度依赖性。对于x = 0、0.05和0.075,获得的直线斜率分别为7.5、12.5和11.44。可以将其与立方系统中磁各向异性的建议值10进行比较[1,6]。指数的偏差是根据二价离子的局部化程度来解释的。

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