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R15Fe78B7的磁晶各向异性
MAGNETOCRYSTALLINE ANISOTROPY OF R15Fe78B7
【摘要】 用磁测量和X-射线衍射方法研究了R15Fe78B7(R=Pr,Nd,Sm,Gd,Y)的磁晶各向异性。发现R=Pr,Gd和Y时,无论室温或低温,c轴都是易磁化方向;R=Sm时,易磁化方向都是在与c轴垂直的基面内;而R=Nd时,易磁化方向随温度变化。在室温时,c轴是易磁化方向,但当温度低于140K时,易磁化方向相对c轴形成一个θ角度。利用Sucksmith-Thompson方法估算了R15Fe78B7的磁晶各向异性常数K1和K2的数值和符号;测量了θ与温度的依赖关系。并通过测定Nd15Fe78B7和Y15Fe78B7的磁晶各向异性及其随温度的变化,进一步分析了Nd15Fe78B7中Nd和Fe不同次点阵对磁晶各向异性的贡献。
【Abstract】 The magnetocrystalline anisotropy of R15Fe78B7(R=Pr, Nd, Sm, Gd and Y) has been studied by magnetic measurement and X-ray diffraction method. A variety of magnetocrystalline anisotropy of R15Fe78B7 has been found. When R=Pr. Gd or Y, the direction of easy magnetization is along the c-axis both at high and low temperature, when R=Sm, it lies in the basal plane perpendicular to c-axis. When R=Nd, it changes with temperature, at room temperature, the direction of easy magnetization is along the c-axis, but below 140K, it deviates from c-axis with an inclinaion angle θ. The anisotropy constants K1 and K2 of R15Fe78B7 have been calculated by using Sucksmith-Thompson’s method and the declination angle θ of Nd15Fe78B7 can be found as a function of temperature. Furthermore, the magnetocrystalline anisotropy and its temperature dependence of Nd and Fe sublattices have been studied by investigating the magnetocrystalline anisotropy of Y15Fe78B7.
- 【文献出处】 中国稀土学报 ,Journal of The Chinese Rare Earth Society , 编辑部邮箱 ,1985年04期
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