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Strong magnetoelectric coupling in mixed ferrimagnetic-multiferroic phases of a double perovskite

机译:双重钙钛矿混合铁磁-多铁相中的强磁电耦合

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摘要

Exploring new magnetic materials is essential for finding advantageous functional properties such as magnetoresistance, magnetocaloric effect, spintronic functionality, and multiferroicity. Versatile classes of double perovskite compounds have been recently investigated because of intriguing physical properties arising from the proper combination of several magnetic ions. In this study, it is observed that the dominant ferrimagnetic phase is coexisted with a minor multiferroic phase in single-crystalline double-perovskite Er2CoMnO6. The majority portion of the ferrimagnetic order is activated by the long-range order of Er3+ moments below TEr = 10 K in addition to the ferromagnetic order of Co2+ and Mn4+ moments arising at TC = 67 K, characterized by compensated magnetization at TComp = 3.15 K. The inverted magnetic hysteresis loop observed below TComp can be described by an extended Stoner–Wohlfarth model. The additional multiferroic phase is identified by the ferroelectric polarization of ~0.9 μC/m2 at 2 K. The coexisting ferrimagnetic and multiferroic phases appear to be strongly correlated in that metamagnetic and ferroelectric transitions occur simultaneously. The results based on intricate magnetic correlations and phases in Er2CoMnO6 enrich fundamental and applied research on magnetic materials through the scope of distinct magnetic characteristics in double perovskites.
机译:探索新的磁性材料对于发现有利的功能特性(如磁阻,磁热效应,自旋电子功能和多铁性)至关重要。由于多种磁性离子的适当结合而产生的令人感兴趣的物理性质,最近研究了多种类型的双钙钛矿化合物。在这项研究中,观察到在单晶双钙钛矿Er2CoMnO6中,主要的亚铁磁性相与次要的多铁磁性相共存。除Co 2 + 的铁磁阶和Er order = 10 K以下的Er 3 + 矩的远位阶激活了亚铁磁阶的大部分,在TC = 67 K时出现Mn 4 + 矩,其特征是在TComp = 3.15 K时补偿了磁化强度,在TComp下方观察到的反向磁滞回线可以用扩展的Stoner-Wohlfarth模型来描述。额外的多铁性相是由在2 K时〜0.9μC/ m 2 的铁电极化确定的,共存的亚铁磁性相和多铁性相似乎是强相关的,因为同时发生了亚磁性和铁电转变。 Er2CoMnO6中复杂的磁相关性和相的结果通过双重钙钛矿中独特的磁性特征的范围丰富了磁性材料的基础和应用研究。

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