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Interaction of Separated Ferromagnetic Domains in a Hole-Doped Manganite Achieved by a Magnetic Field

机译:磁场实现的掺杂空穴的锰矿中分离铁磁畴的相互作用

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摘要

We report the change in the magnetic microstructure with the application of a magnetic field to a hole-doped manganite La_(0.81)Sr_(0.19)MnO_3 in the mixed-phase state, in which ferromagnetic and paramagnetic phases coexist In situ observations by electron holography have revealed that the applied magnetic field generates a "channel" of the magnetic flux in the paramagnetic phase region, thereby connecting the separated ferromagnetic domains. The magnetic flux density of this channel is estimated at 0.33 T, which is comparable with that of the ferromagnetic domains. The connection of the separated ferromagnetic domains appears to promote the conduction in the mixed-phase state as predicted for many manganites exhibiting the magnetoresistance effect.
机译:我们报告了在混合相状态下,磁场掺杂到掺杂有孔的锰矿La_(0.81)Sr_(0.19)MnO_3中的磁性微观结构的变化,其中铁磁和顺磁相共存于电子全息原位观察已经揭示出所施加的磁场在顺磁相区域中产生磁通量的“通道”,从而连接分离的铁磁畴。该通道的磁通密度估计为0.33 T,与铁磁畴的磁通密度相当。正如许多表现出磁阻效应的锰矿所预测的那样,分离的铁磁畴的连接似乎促进了混合相状态下的导电。

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