首页> 外文会议>NATO Advanced Research Workshop on Magnetic Resonance in Colloid and Interface Science, Jun 26-30, 2001, St.Petersburg, Russia >ORBITAL ORDER AND ORBITAL FLUCTUATIONS IN COLOSSAL MAGNETORESISTIVE MANGANITES. AN INVESTIGATION WITH ~(55)Mn AND ~(139)La NMR
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ORBITAL ORDER AND ORBITAL FLUCTUATIONS IN COLOSSAL MAGNETORESISTIVE MANGANITES. AN INVESTIGATION WITH ~(55)Mn AND ~(139)La NMR

机译:整体磁阻锰矿的轨道次序和轨道波动。 〜(55)Mn和〜(139)La NMR的研究

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~(55)Mn and ~(139)La NMR techniques are shown to be an excellent tool for detecting changes in the local electronic properties of colossal magnetoresistance manganites. Based on this we discuss the possibility of detecting orbital ordering in ferromagnetic La_(1-x)Ca_xMnO3 (0.20≤_x<0.5). We also provide evidence about the formation of an unusual kind of phase separation in the low temperature regime of the ferromagnetic conductive regime of the magnetic phase diagram for x≥0.25. Specifically, we show that by lowering temperature, an extra NMR signal is formed in the ferromagnetic conductive phase, which originates from regions with extremely small magnetic anisotropy, possibly produced by strong orbital fluctuations.
机译:〜(55)Mn和〜(139)La NMR技术显示出是检测巨大磁阻锰矿局部电子性质变化的极佳工具。基于此,我们讨论了检测铁磁La_(1-x)Ca_xMnO3(0.20≤_x<0.5)中轨道有序的可能性。我们还提供了有关x≥0.25的磁性相图的铁磁导电态的低温态中异常相分离形式的形成的证据。具体而言,我们表明,通过降低温度,铁磁导电相中会形成额外的NMR信号,该信号源自磁各向异性极小的区域,可能是由强烈的轨道波动产生的。

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