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铁基-稀土赝三元磁性化合物的磁性及磁性交互作用
赵志刚
学位类型硕士
导师庄育智
1990
学位授予单位中国科学院金属研究所
学位授予地点中国科学院金属研究所
摘要本文利用X射线衍射仪、交流初始磁化率测量仪、脉冲强磁场测量仪、提拉样品磁强计等测量设备对(Nd,Pr)_2 (Fe,Co)_(14)B化合物的基础磁性及磁性交互作用进行了研究。结果表明Nd_2Fe_(14)B化合物低温下存在有自旋再取向的同时,伴随有晶体的X射线衍射强度的反常。这种反常是由于其晶体的反常热膨胀所造成的。部分Pr替代Nd使得(Nd_(1-x)Pr_x)_2Fe_(14)B化合物表现出复杂的磁学性质。这种现象被归因于Pr离子的价态不稳定性,由此导致化合物中稀土亚晶格对磁晶各向异性的贡献偏离单离子模型。高场磁化测量结果表明在4.2K下,(Nd_(1-x)Pr_x)_2Co_(14)B化合物存在有一级磁化过程(FOMP),导致Pr_2Co_(14)B化合物此温度下的磁晶各向异性场仅为49T,远小于文献报导的75T。在(Nd,Pr)_2 (Fe,Co)_(14)B化合物中,Pr替代Nd使得4f-3d交互作用降低;Co的加入使Pr,Nd亚晶格4f-3d交互作用的差别减小。相反,使Pr,Nd亚晶格对磁晶各向异性贡献的差别增大。
其他摘要Structure, magnetic properties and magnetic interaction have been studied for (Nd,Pr)_2 (Fe,Co)_(14)B compounds with X-ray diffraction, AC-Susceptibility and high pulse magnetic field tech. etc. From theseexperiments one can realized that at the spin-reorienation temperature of Nd_2Fe_(14)B compound, X-ray diffraction strength show an abnormal which can be associated with abnormal thermal expansition of lattice of Nd_2Fe_(14)B at low temperature. Partial substitution of Pr for Nd makes magnetic behavior of (Nd_(1-x)Pr_x)_2Fe_(14)B compounds very complicated, and this phenomenon has been attributed to the valence instability of Pr ions in these compounds. Due to the reason mentionedabove, the contrinution to the magnetocrystalline anisotropy from 4f sublattice of the compounds may deviated from Single Ion Model. From experimental results of the high field magnetization, it brings to a conclusion that first order magnetization process (FOMP) exists in all (Nd_(1-x)Pr_x)_2Co_(14)B compounds at T = 4.2 K, and as a consequence, the magnetocrystalline anisotropy field of Pr_2Co_(14)B compound can be only about 49T at T = 4.2K, which is much lower than the published result 75T. It was also found that in (Nd,Pr)_2 (Fe,Co)_(14)B compounds, Partial substitution of Pr for Nd led todecrease of 4f-3d exchange interaction; substitution of Co for Fe made the difference of 4f-3d exchange interaction of Pr and Nd sublattice lower, meanwhile it made the difference of the magnetocrystalline anisotropy of the two sublattice go up.
页数121
语种中文
文献类型学位论文
条目标识符http://ir.imr.ac.cn/handle/321006/17451
专题中国科学院金属研究所
推荐引用方式
GB/T 7714
赵志刚. 铁基-稀土赝三元磁性化合物的磁性及磁性交互作用[D]. 中国科学院金属研究所. 中国科学院金属研究所,1990.
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