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Magnetism-Driven Ferroelectricity in Double Perovskite Y2NiMnO6

机译:双钙钛矿Y2NiMnO6中的磁驱动铁电

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We report the discovery of multiferroic behavior in double perovskite Y2NiMnO6. X-ray diffraction shows that the material has a centrosymmetric crystal. structure of space group P2(1) with Ni2+/Mn4+ Ordering. This result is further confirmed by aberration-corrected scanning transmission electron microscopy combined with atomic resolution electron energy loss spectroscopy. The appearance of ferroelectric polarization. coincides with the magnetic phase transition (similar to 67 K), which indicates that the ferroelectricity is driven by magnetism, and this is further confirmed by its strong Magnetoelectric (ME) effect. We proposed the origin of the ferro electricity is associated with the combination of Ni2+/Mn4+ charge ordering and the up arrow up arrow down arrow down arrow spin ordering. When compared with other known magnetic multiferroics, Y2NiMnO6 displays several attractive multiferroic properties, including high polarization (similar to 145 mu C/m(2)), a high multiferroic transition temperature (similar to 67 K), and strong ME coupling (similar to 21%).
机译:我们报道了在双钙钛矿Y2NiMnO6中多铁性行为的发现。 X射线衍射表明该材料具有向心对称的晶体。 Ni2 + / Mn4 +有序的空间群P2(1)/ n的结构。通过像差校正的扫描透射电子显微镜结合原子分辨率电子能量损失谱进一步证实了该结果。铁电极化的出现。与磁相变(类似于67 K)一致,这表明铁电是由磁性驱动的,这还可以通过其强大的磁电(ME)效应得到进一步证实。我们提出铁电的起源与Ni2 + / Mn4 +电荷排序和向上箭头向上箭头,向下箭头向下箭头向下旋转的组合相关。与其他已知的磁性多铁相比较,Y2NiMnO6具有多种吸引人的多铁性能,包括高极化(类似于145μC / m(2)),高多铁转变温度(类似于67 K)和强ME耦合(类似于21%)。

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