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Griffiths phase and the magnetic and transport properties of doped manganites

机译:格里菲斯相与掺杂锰铁矿的磁性和输运性质

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A phenomenological model is proposed to describe the magnetic and magnetoresistance properties of ferromagnetic manganites. This model is based on the methods used to describe hysteretic systems, takes into account phase separation effects, and assumes the transition of ferromagnetic manganites into the Griffiths phase at above the Curie temperature. This formalism makes it possible to describe the conducting properties of the systems in the temperature range from low temperatures to the Griffiths temperature (T _G). This approach is used to qualitatively explain the experimental laws of the behavior of ferromagnetic manganites using the temperature and field dependences of the electrical resistivity and magnetization, the hysteretic properties, and the magnetoresistive effect (MRE) and to classify manganites in the magnitude of the MRE. The parameter that is responsible for the response of a system to thermal effects is the ratio of the maximum energy barrier separating various states of a system at zero temperature W _A (0) to thermal fluctuation energy W _(Cfl) at T _G. The W _A (0)/W _(Cfl) ratio is found to determine the temperature range of the Griffiths phase. The relation between the magnitudes of the MRE and parameter W _A (0)/W _(Cfl) for a certain system is revealed. The behavior of the magnetization and electrical resistivity of manganites in the Griffiths phase is discussed.
机译:提出了一种现象学模型来描述铁磁锰矿的磁阻特性。该模型基于描述迟滞系统的方法,考虑了相分离效应,并假设在居里温度以上,铁磁锰矿过渡到格里菲斯相。这种形式主义使得可以描述从低温到格里菲斯温度(T _G)的温度范围内系统的导电特性。该方法用于通过电阻率和磁化强度,磁滞特性和磁阻效应(MRE)的温度和场依赖性来定性地解释铁磁锰矿行为的实验规律,并根据MRE的大小对锰矿进行分类。 。负责系统对热效应响应的参数是在零温度W _A(0)时分隔系统各种状态的最大能垒与T _G处的热波动能W _(Cfl)之比。发现W_A(0)/ W_(Cfl)之比确定格里菲斯相的温度范围。对于特定系统,揭示了MRE的大小与参数W_A(0)/ W_(Cfl)之间的关系。讨论了格里菲斯相中锰矿的磁化和电阻率行为。

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