Baños-López Esperanza, Sánchez-De Jesús Félix, Cortés-Escobedo Claudia A, Barba-Pingarrón Arturo, Bolarín-Miró Ana María
Área Académica de Ciencias de la Tierra y Materiales, Universidad Autónoma del Estado de Hidalgo, Mineral de la Reforma, Hidalgo 42184, Mexico.
Centro de Investigación e Innovación Tecnológica, Instituto Politécnico Nacional, Azcapotzalco, Ciudad de México 02250, Mexico.
Materials (Basel). 2018 Sep 7;11(9):1652. doi: 10.3390/ma11091652.
The effect of the substitution of Y by Nd on the structural and magnetic properties of neodymium-doped yttrium iron garnet, NdYFe₅O with 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 NdYFe₅O (0 ≤ ≤ 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 Nd into the garnet structure with a neodymium doping concentration () of 0⁻2.0, which causes a consistent increment in the lattice parameters with the Nd content. When 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 Nd increases, while there was enhanced saturation magnetization as well as modified remanence and coercivity with respect to non-doped YIG.
本文介绍了用钕替代钇对钕掺杂钇铁石榴石(NdYFe₅O,其中钕含量范围为0⁻2.5)结构和磁性的影响。将Fe₂O₃、Nd₂O₃和Y₂O₃的氧化物粉末按化学计量比混合,使用高能球磨研磨5小时,然后在900 MPa下单轴压制,并在1373 K下退火2小时,以获得NdYFe₅O(0≤≤2.5)。研究发现,对氧化物进行机械研磨后再退火有助于石榴石结构的完全形成。此外,X射线衍射图谱证实钕以0⁻2.0的钕掺杂浓度()完全引入石榴石结构,这导致晶格参数随钕含量持续增加。当大于2.0时,正铁酸钇成为主要相。此外,磁性结果表明,随着钕含量的增加,居里温度升高(583 K),同时相对于未掺杂的钇铁石榴石,饱和磁化强度增强,剩磁和矫顽力也发生了变化。