4.7 Article

Influence of Fe3+by La3+cations substitution on the crystallography and magnetic properties of yttrium iron garnet compound

期刊

CERAMICS INTERNATIONAL
卷 49, 期 16, 页码 27567-27576

出版社

ELSEVIER SCI LTD
DOI: 10.1016/j.ceramint.2023.06.032

关键词

La-doped yttrium iron garnet; Rietveld refinement; Charge distribution; Electronic microscopy; Magnetic properties

向作者/读者索取更多资源

In this study, the influence of La3+ cations insertion on the crystallography, morphology, and magnetic properties of Y3Fe5-xLaxO12 compound was investigated using the sol-gel method. The Rietveld refinement method was used to confirm the Fe3+ by La3+ cations replacement and quantify the structural parameters. The results showed that La3+ cations insertion significantly affected the lattice constant, crystallite size, microstrain, sites occupancy, bond angles and distances of the YIG crystal structure.
In the present study, we have investigated the influence of La3+ cations insertion on the crystallography, morphology, and magnetic properties of Y3Fe5-xLaxO12 compound, (x = 0.00 and 0.03) obtained by the sol-gel method. To confirm the Fe3+ by La3+ cations replacement and quantify the structural parameters, the Rietveld refinement method was used. The quantitative analysis confirmed that, the La3+ cations insertion in the YIG crystal structure affect significative the lattice constant, crystallite size, microstrain, sites occupancy, bond angles and distances. Room temperature Raman spectra also confirmed the YIG single phase structure. The spectra deconvolution pointed shifts for smaller wavenumber in the sample containing La3+ cations, specifically in the region between 400 and 800 cm-1, correlated with the octahedral and tetrahedral sites. The coral format morphology was confirmed by Scanning and Transmission Electron Microscopies. Lastly, room temperature magnetic measurements demonstrated that the La3+ cations insertion in the YIG crystal structure, provokes an increase in the saturation magnetization (Ms), remanent magnetization (Mr) and magnetocrystalline anisotropy (K1) of 24.8, 17.5, and 9.3%, respectively, respect to the values obtained for undoped YIG sample.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据