首页> 外文期刊>Journal of magnetism and magnetic materials >Uncompensated-spins induced weak ferromagnetism in Ca_3Mn_2O_7: Magneto-conductive and dual magneto-capacitive effects
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Uncompensated-spins induced weak ferromagnetism in Ca_3Mn_2O_7: Magneto-conductive and dual magneto-capacitive effects

机译:未补偿自旋在Ca_3Mn_2O_7中感应弱铁磁性:磁导和双磁电容效应

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摘要

Temperature dependent magnetization study on single phase orthorhombic Ruddlesden-Popper manganite Ca3Mn2O7 evidences antiferromagnetic (AFM) ordering below 123 K. Field-dependent magnetization M(H) depicts off-centered hysteretic loops below similar to 110 K-confirming the existence of both weak ferromagnetism (WFM) and exchange bias, whose development upon cooling is examined in detail. WFM is attributed to the formation of uncompensated-spin-clusters within the AFM-matrix, stabilized by the high-anisotropy in the manganite, favoring Dzyaloshinskii-Moriya (D-M) interaction. Temperature dependence of an evaluated average canting angle from the M(H) loops provides a quantitative measure of the WFM-evolution. Dielectric measurements exhibit magneto-conductive effects concurrent to the WFM-onset. Temperature dependence of the low-frequency/dc-limit of Jonscher-fits to the conductivity isotherms confirms the presence of relatively more-conductive clusters, embedded in the insulating-bulk. Nyquist impedance-analysis of complex impedance reveals two relaxations, yielding dual magnetic-field effects; the lumped circuit parameters feature anomalies across the magnetic phase changes.
机译:对单相正交各向异性Ruddlesden-Popper锰矿Ca3Mn2O7的温度依赖性磁化研究表明,反铁磁(AFM)有序在123 K以下。磁场相关磁化M(H)表示低于110 K的偏心磁滞回线,这表明两种弱铁磁性都存在(WFM)和交换偏差,详细研究了冷却后其发展。 WFM归因于AFM矩阵内无补偿自旋团簇的形成,并通过锰矿中的高各向异性来稳定,有利于Dzyaloshinskii-Moriya(D-M)相互作用。来自M(H)回路的评估平均倾斜角度的温度依赖性提供了WFM演变的定量度量。介电测量显示出与WFM发生同时发生的磁导效应。 Jonscher拟合的低频/直流极限对电导率等温线的温度依赖性证实了存在于绝缘体中的相对导电性更高的簇的存在。复阻抗的奈奎斯特阻抗分析显示出两种弛豫,产生双重磁场效应。集总电路参数在整个磁相位变化中具有异常特征。

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