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Intrinsic inhomogeneities of low-doped lanthanum manganites in the paramagnetic temperature range

机译:在顺磁温度范围内低掺杂镧锰的固有非均质性

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The nature of the electrical resistivity for low-doped lanthanum manganites is elucidated. The electrical resistivity is described by the Efros-Shklovskii law (inρ ~∞ (T _0/T) ~(-1/2), where T _0 ~∞ 1/R _(is)) in the temperature range from T* ≈ 300 K ≈ T _C (T _C is the Curie temperature for conducting manganites) to their T _C and is explained by the tunneling of carriers between localized states. The magnetoresistance is explained by a change in the size of localized states R _(is) in a magnetic field. The patterns of change in R _(is) with temperature and magnetic field strength determined from magnetotransport properties are satisfactorily described in the model of phase separation into small-radius metallic droplets in a paramagnetic matrix. The sizes R _(is) and their temperature dependence have been estimated through magnetic measurements. The results confirm the existence of a Griffith phase. The intrinsic inhomogeneities produced by thermodynamic phase separation determine the electrical resistivity and magnetoresistance of lanthanum manganites.
机译:阐明了低掺杂镧锰矿的电阻率性质。电阻率由Efros-Shklovskii定律(inρ〜∞(T _0 / T)〜(-1/2),其中T _0〜∞1 / R _(is))在T *的温度范围内描述。 300 K≈T _C(T _C是传导锰的居里温度)达到其T _C,这可以通过局部态之间的载流子隧穿来解释。磁阻通过磁场中局部状态R _(is)的大小变化来解释。在顺磁性基质中相分离成小半径金属液滴的模型中,令人满意地描述了R_(is)随温度和磁场强度的变化模式,该变化是由磁传输性质确定的。尺寸R_(is)及其温度依赖性已经通过磁性测量来估计。结果证实了格里菲斯相的存在。由热力学相分离产生的内在不均匀性决定了镧锰的电阻率和磁阻。

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