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The Verwey transition observed by spin-resolved photoemission electron microscopy

机译:通过自旋分辨光电子显微镜观察到的Verwey跃迁

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We have imaged the magnetic domains on magnetite (001) through the Verwey transition by means of spin-resolved photoemission electron microscopy. A He laboratory source is used for illumination. The magnetic domains walls above the Verwey transition are aligned with < 110 > in-plane directions. Below the Verwey transition, the domain structure is interpreted as arising from a distribution of areas with different monoclinic c-axis, with linear 180 degrees domain walls within each area and ragged edges when the magnetic domain boundaries coincide with structural domain walls. The domains evolve above the Verwey transition, while they are static below. (C) 2016 Elsevier B.V. All rights reserved.
机译:我们已经通过自旋分辨光发射电子显微镜通过Verwey跃迁对磁铁矿(001)上的磁畴成像。氦气实验室光源用于照明。 Verwey过渡上方的磁畴壁与<110>面内方向对齐。在Verwey跃变以下,磁畴结构被解释为是由具有不同单斜c轴的区域分布引起的,当磁畴边界与结构磁畴壁重合时,每个区域内的线性180度磁畴壁和参差不齐的边缘。这些域在Verwey转换之上演化,而在下面是静态的。 (C)2016 Elsevier B.V.保留所有权利。

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