Site-selective cobalt substitution in La–Co co-substituted magnetoplumbite-type ferrites: 59Co-NMR and DFT calculation study

Hiroyuki Nakamura, Hiroto Ohta, Ryuya Kobayashi, Takeshi Waki, Yoshikazu Tabata, Hidekazu Ikeno and Christian Mény
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Abstract

The La–Co co-substituted magnetoplumbite-type (M-type) ferrites AFe12O19 (A = Ca, Sr and Ba, ion sizes Ca2+ Sr2+ Ba2+) with Co compositions around 0.2 have been subjected to 59Co-NMR. The results show that Co occupies the 4f1, 2a and 12k sites, and that the smaller the A ion, the more Co tends to occupy the 4f1 minority spin site, which is effective in enhancing both uniaxial anisotropy and magnetisation. First-principles total energy calculations based on density functional theory (DFT) of undoped AFe12O19 and a supercell ( of the unit cell) in which 1/96 of Fe3+ is replaced by Co2+ were performed to predict the stable structure and Co occupancy sites. The results show that regardless of A, Co is most stable when it occupies the 4f1 site, followed by the 2a and 12k sites with energy differences on the order of 100 meV, and Co practically does not occupy the 2b and 4f2 sites. As the A ion becomes smaller, the energy difference when Co occupies each Fe site tends to increase, and the Co occupancy of the 4f1 site also increases. The site selectivity of Co can be roughly explained as a result of the difference in uniaxial strain along the c-axis associated with the difference in A. However, the influence of the A ion differs between the R and S blocks and the local strain also has a secondary effect on the Co distribution. Based on these results, the guidelines for improving the performance (anisotropy and magnetisation) of La–Co co-substituted M-type ferrite magnets with a limited amount of Co can be summarised as follows: It is effective to select as small A ions as possible and to post-anneal at low temperature or cool slowly to concentrate Co at the 4f1 site in tetrahedral coordination.
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La-Co 共取代磁铌铁氧体中钴的位点选择性取代:59Co-NMR 和 DFT 计算研究
对 Co 含量在 0.2 左右的 La-Co 共取代磁铌铁(M 型)铁氧体 AFe12O19(A = Ca、Sr 和 Ba,离子大小为 Ca2+ Sr2+ Ba2+)进行了 59Co-NMR 分析。结果表明,钴占据了 4f1、2a 和 12k 位点,而且 A 离子越小,钴就越倾向于占据 4f1 少数自旋位点,从而有效地增强了单轴各向异性和磁性。我们基于密度泛函理论(DFT)对未掺杂的 AFe12O19 和用 Co2+ 取代了 1/96 的 Fe3+ 的超晶胞(单位晶胞)进行了第一原理总能量计算,以预测其稳定结构和 Co 占有位点。结果表明,无论 A 如何,Co 在占据 4f1 位点时最稳定,其次是 2a 和 12k 位点,能量差在 100 meV 量级,Co 几乎不占据 2b 和 4f2 位点。随着 A 离子变小,Co 占据每个 Fe 位点时的能量差趋于增大,Co 占据 4f1 位点的能量差也随之增大。Co 的位点选择性可大致解释为与 A 离子差异相关的沿 c 轴的单轴应变差异的结果,但 A 离子的影响在 R 块和 S 块之间有所不同,局部应变也会对 Co 的分布产生次要影响。基于这些结果,使用少量 Co 改善 La-Co 共取代 M 型铁氧体磁体性能(各向异性和磁化)的指导原则可归纳如下:选择尽可能小的 A 离子,并在低温下进行后退火或缓慢冷却以将 Co 集中在四面体配位的 4f1 位点,这样做是有效的。
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