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arXiv 2402.09706cond-mat.mtrl-sci
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La-Co共取代磁铅矿石型铁氧体中的Co位选择性取代:$^{59}$Co-NMR和DFT计算研究

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

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

AI总结:

通过$^{59}$Co-NMR和DFT计算研究La-Co共取代M型铁氧体中Co的位点选择性,发现选择较小$A$离子并低温退火可将Co集中于4f$_1$位点,从而增强各向异性和磁化。

摘要:

La-Co共取代的磁铅矿石型(M型)铁氧体$A$Fe$_{12}$O$_{19}$($A$ = Ca, Sr和Ba,离子尺寸Ca$^{2+}$ $<$ Sr$^{2+}$ $<$ Ba$^{2+}$,Co组成约为0.2)已进行了$^{59}$Co-NMR测试。结果表明,Co占据4f$_1$、2a和12k位点,且$A$离子越小,Co越倾向于占据4f$_1$11}$少数自旋位点,这有助于增强单轴各向异性和磁化。基于密度泛函理论(Dft)的第一性原理总能量计算,用于预测未掺杂$A$Fe$_{12}$O$_{19}$及超胞(unit cell的$2 \ imes 2 \ imes 1$,其中1/96的Fe$^{3+}$被Co$^{2+}$取代)以进行,预测稳定结构和Co占据位点。结果表明,无论$A$为何,Co占据44f$_1$位点时最稳定,其次是2a和12k位点,能量差约为100 meV,Co实际上不占据2b和4f$_2$位点。随着$A$离子变小,Co占据各Fe位点时的能量差趋于增大,4f$_1$位点的Co占据率也增加。Co的位点选择性可粗略解释为与$A$差异相关的沿$c$轴单轴应变差异的结果。然而,$A$离子的影响在R和S块间不同,局部应变对Co分布也有次要影响。基于这些结果,改进含限量Co的La-Co共取代M型铁氧体磁体性能(各向异性和磁化)的指南可总结如下:选择尽可能小的$A$离子,并在低温后退火或缓慢冷却以将Co集中于四面体配位的4f$_1$位点,是有效的。

英文摘要:

The La-Co co-substituted magnetoplumbite-type (M-type) ferrites $A$Fe$_{12}$O$_{19}$ ($A$ = Ca, Sr and Ba, ion sizes Ca$^{2+}$ $<$ Sr$^{2+}$ $<$ Ba$^{2+}$) with Co compositions around 0.2 have been subjected to $^{59}$Co-NMR. The results show that Co occupies the 4f$_1$, 2a and 12k sites, and that the smaller the $A$ ion, the more Co tends to occupy the 4f$_1$ 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 $A$Fe$_{12}$O$_{19}$ and a supercell ($2 \times 2 \times 1$ of the unit cell) in which 1/96 of Fe$^{3+}$ is replaced by Co$^{2+}$ 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 4f$_1$ 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 4f$_2$ 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 4f$_1$ 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 4f$_1$ site in tetrahedral coordination.

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