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Enhancement in Curie Temperature of Yttrium Iron Garnet by Doping with Neodymium

机译:掺钕提高钇铁石榴石的居里温度

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摘要

The effect of the substitution of Y3+ by Nd3+ on the structural and magnetic properties of neodymium-doped yttrium iron garnet, NdxY3−xFe5O12 with x in the range of 0–2.5, is presented. Oxide powders of Fe2O3, Nd2O3, and Y2O3 were mixed in a stoichiometric ratio and milled for 5 h using high-energy ball milling, before being uniaxially pressed at 900 MPa and annealed at 1373 K for 2 h to obtain NdxY3−xFe5O12 (0 ≤ x ≤ 2.5). It was found that the mechanical milling of oxides followed by annealing promotes the complete structural formation of the garnet structure. Additionally, the X-ray diffraction patterns confirm the complete introduction of Nd3+ into the garnet structure with a neodymium doping concentration (x) of 0–2.0, which causes a consistent increment in the lattice parameters with the Nd3+ content. When x is higher than 2.0, the yttrium orthoferrite is the predominant phase. Besides, the magnetic results reveal an increase in the Curie temperature (583 K) as the amount of Nd3+ increases, while there was enhanced saturation magnetization as well as modified remanence and coercivity with respect to non-doped YIG.
机译:用Nd 3 + 代替Y 3 + 对掺钕钇钇铁石榴石NdxY3-xFe5O12的结构和磁性的影响呈现0–2.5。将Fe2O3,Nd2O3和Y2O3的氧化物粉末以化学计量比混合并使用高能球磨机研磨5小时,然后在900 MPa下单轴加压并在1373 K退火2小时以获得NdxY3-xFe5O12(0≤ x≤2.5)。已经发现,氧化物的机械研磨然后退火可以促进石榴石结构的完整结构形成。此外,X射线衍射图证实钕掺杂浓度(x)为0-2.0时,将Nd 3 + 完全引入到石榴石结构中,这导致晶格参数随Nd 3 + 的内容。当x大于2.0时,钇铁素体为主要相。此外,磁学结果表明居里温度(583 K)随着Nd 3 + 的增加而增加,而饱和磁化强度增强,并且相对于非磁性材料,剩磁和矫顽力得到了改善。掺杂的YIG。

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