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首页> 外文期刊>Journal of the European Ceramic Society >Magnetic properties of Er(Co, Mn)O_3 perovskites
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Magnetic properties of Er(Co, Mn)O_3 perovskites

机译:Er(Co,Mn)O_3钙钛矿的磁性

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The erbium-based manganite ErMnO_3 has been partially substituted at the manganese site by Co in the general formula ErCo_xMn_(1-x)O_3. The perovskite orthorhombic structure is found fromx(Co) = 0.3 up to x(Co) = 0.7, provided that the synthesis is performed under oxygenation conditions to favour the presence of Co~(3+). Magnetic properties show unusual phenomena, correlated with the presence of different magnetic entities (i.e., Er~(3+), Co~(2+), Co~(3+), Mn~(3+), Mn~(4+)): the overall magnetic moment reverses its sign when the sample is cooled under an external magnetic field, while the magnetization loops performed at T<4K show intersecting branches at low fields and a sudden jump at high fields. A phenomenological model of two interacting sublattices, coupled by an antiferromagnetic exchange interaction, explains the inversion of the overall spin, while the high-field discontinuity is explained in terms of dynamical models.
机译:the基锰矿ErMnO_3在锰部位被通式ErCo_xMn_(1-x)O_3的Co部分取代。钙钛矿的正交晶结构从x(Co)= 0.3到x(Co)= 0.7,前提是在氧化条件下进行合成以有利于Co〜(3+)的存在。磁性表现出不寻常的现象,与不同的磁性实体(即Er〜(3 +),Co〜(2 +),Co〜(3 +),Mn〜(3 +),Mn〜(4+ )):当样品在外部磁场下冷却时,总磁矩反转其符号,而在T <4K时执行的磁化回路在低磁场下显示相交分支,在高磁场下突然跳变。由反铁磁交换相互作用耦合的两个相互作用的子晶格的现象模型解释了整个自旋的反演,而高场的不连续性则用动力学模型解释了。

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