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Comparison of coherent and weakly incoherent transport models for the interlayer magnetoresistance of layered Fermi liquids

机译:相干和弱相干传输模型的比较   层状费米液体的层间磁阻

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摘要

The interlayer magnetoresistance of layered metals in a tilted magnetic fieldis calculated for two distinct models for the interlayer transport. The firstmodel involves coherent interlayer transport and makes use of results ofsemi-classical or Bloch-Boltzmann transport theory. The second model involvesweakly incoherent interlayer transport where the electron is scattered manytimes within a layer before tunneling into the next layer. The results arerelevant to the interpretation of experiments on angular-dependentmagnetoresistance oscillations (AMRO) in quasi-one- and quasi-two-dimensionalmetals. We find that the dependence of the magnetoresistance on the directionof the magnetic field is identical for both models except when the field isalmost parallel to the layers. An important implication of this result is thata three-dimensional Fermi surface is not necessary for the observation of theYamaji and Danner oscillations seen in quasi-two- and quasi-one-dimensionalmetals, respectively. A universal expression is given for the dependence of theresistance at AMRO maxima and minima on the magnetic field and scattering time(and thus the temperature). We point out three distinctive features of coherentinterlayer transport: (i) a beat frequency in the magnetic oscillations ofquasi-two-dimensional systems, (ii) a peak in the angular-dependentmagnetoresistance when the field is sufficiently large and parallel to thelayers, and (iii) a crossover from a linear to a quadratic field dependence forthe magnetoresistance when the field is parallel to the layers. Properties (i)and (ii) are compared with published experimental data for a range ofquasi-two-dimensional organic metals and for Sr2RuO4.
机译:针对两个不同的层间传输模型,计算了倾斜磁场中层状金属的层间磁阻。第一个模型涉及相干的层间传输,并利用半经典或Bloch-Boltzmann传输理论的结果。第二种模型涉及弱的非相干层间传输,其中电子在隧穿进入下一层之前在一层内多次散射。该结果与准一维和准二维金属的角度相关磁阻振荡(AMRO)实验的解释有关。我们发现,两个模型的磁阻对磁场方向的依赖性相同,除了当磁场几乎平行于各层时。该结果的重要含义是,对于观察分别在准二维和准一维金属中看到的雅马吉和丹纳振荡,不需要三维费米表面。对于在最大和最小AMRO处的电阻对磁场和散射时间(以及温度)的依赖性,给出了一个通用表达式。我们指出了相干层间传输的三个显着特征:(i)准二维系统的磁振荡中的拍频;(ii)当磁场足够大且平行于层时,与角度相关的磁阻的峰值;以及( iii)当磁场平行于层时,磁阻从线性场到二次场的转换。将性质(i)和(ii)与一系列准二维有机金属和Sr2RuO4的公开实验数据进行比较。

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  • 年度 1999
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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