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Magnetization Anisotropy in Amorphous Nd_8Fe_(86)B_6 Ribbons

Magnetization Anisotropy in Amorphous Nd_8Fe_(86)B_6 Ribbons
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摘要 Crystalline, partial and complete amorphous Nd_8Fe_(86)B_6 ribbons were prepared by melt spinning with different wheel speeds from 7 to 43 m·s^(-1). All the ribbons exhibited anisotropy in magnetization, which unusually increased when the ribbons changed from crystalline to amorphous states and slightly decreased when the quenching speeds were higher than 38 m·s^(-1). The experiments reveal that the anisotropy of amorphous ribbons is inherited after crystallization. It is understood that the anisotropy in magnetization of amorphous Nd_8Fe_(86)B_6 ribbons is responsible for the preferred orientation of spontaneous magnetization vectors of Nd-Fe-B clusters. Crystalline, partial and complete amorphous Nd_8Fe_(86)B_6 ribbons were prepared by melt spinning with different wheel speeds from 7 to 43 m·s^(-1). All the ribbons exhibited anisotropy in magnetization, which unusually increased when the ribbons changed from crystalline to amorphous states and slightly decreased when the quenching speeds were higher than 38 m·s^(-1). The experiments reveal that the anisotropy of amorphous ribbons is inherited after crystallization. It is understood that the anisotropy in magnetization of amorphous Nd_8Fe_(86)B_6 ribbons is responsible for the preferred orientation of spontaneous magnetization vectors of Nd-Fe-B clusters.
机构地区 School of Science
出处 《Journal of Rare Earths》 SCIE EI CAS CSCD 2004年第S1期95-98,共4页 稀土学报(英文版)
基金 theNationalNaturalScienceFoundationofChina (5 0 2 710 5 1)
关键词 ND-FE-B magnetic anisotropy MELT-SPUN AMORPHOUS rare earths Nd-Fe-B magnetic anisotropy melt-spun amorphous rare earths
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