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First order spin flop transition in yttrium iron garnet (YIG)

机译:钇铁石榴石(YIG)的一阶旋转跳变

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We have studied the field dependence of the sublattice magnetization of ferrimagnetic yttrium iron garnet (YIG) using neutron scattering. In contrast to the macroscopic spontaneous magnetization that shows the normal field dependence of a soft ferromagnet (sudden saturation at the demagnetization field and no hysteresis) in neutron scattering a field induced first order spin flop transition with considerable hysteresis is observed at a critical field of H_c ~ 580 G (external field). Considering that with neutron scattering the antiferromagnetic component of ~4/5 of the total moment is detected preferentially while in the macroscopic magnetization samples the ferromagnetic component of ~ 1/5 exclusively it becomes clear that ferromagnetic and antiferromagnetic component have a completely independent field (and temperature) dependence. This indicates that the two magnetic structures have to be viewed as two weakly coupled order parameters. In the zero field ground state the moment orientations of the two ordering structures are orthogonal. Only for fields H_0 > H_c a nearly collinear ferrimagnetic order is established by the field.
机译:我们已经使用中子散射研究了亚铁钇铁石榴石(YIG)的亚晶格磁化强度的场相关性。与宏观自发磁化相反,后者显示中子散射中软铁磁体的正常磁场依赖性(在退磁磁场中突然饱和并且没有磁滞),在H_c的临界场处观察到具有相当大的磁滞的磁场诱导的一阶自旋跃迁跃迁。 〜580 G(外场)。考虑到中子散射会优先检测到总力矩的〜4/5的反铁磁成分,而在宏观磁化样本中,铁磁成分的〜1/5排他地被发现,显然铁磁和反铁磁成分具有完全独立的场(并且温度)依赖性。这表明必须将两个磁性结构视为两个弱耦合的阶跃参数。在零场基态下,两个有序结构的矩方向是正交的。仅对于磁场H_0> H_c,磁场才能建立几乎共线的亚铁磁阶。

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