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从天然陨石中提取的L1 0型有序FeNi合金的结构、磁性和电子态表征

Structural, magnetic and electronic state characterization of L1 0-type ordered FeNi alloy extracted from a natural meteorite.

作者信息

Kotsugi M, Maruyama H, Ishimatsu N, Kawamura N, Suzuki M, Mizumaki M, Osaka K, Matsumoto T, Ohkochi T, Ohtsuki T

出版信息

J Phys Condens Matter. 2014 Feb 12;26(6):064206. doi: 10.1088/0953-8984/26/6/064206.

Abstract

To understand the hard magnetism of L10-type ordered FeNi alloy, we extracted the L10-FeNi phase from a natural meteorite, and evaluated its fundamental solid-state properties: sample composition, magnetic hysteresis, crystal structure and electronic structure. We executed multidirectional analyses using scanning electron microscopy with an electron probe micro-analyzer (SEM-EPMA), a superconducting quantum interference device (SQUID), x-ray diffraction (XRD) and magnetic circular dichroism (MCD). As a result, we found that the composition was Fe: 50.47 ± 1.98 at.%, Ni: 49.60 ± 1.49 at.%, and an obvious superlattice peak is confirmed. The estimated degree of order was 0.608, with lattice constants a = b = 3.582 Å and c = 3.607 Å. The obtained coercivity was more than 500 Oe. MCD analysis using the K absorption edge suggests that the magnetic anisotropy could originate from the orbital magnetic moment of 3d electrons in Fe; this result is consistent with that in a previous report obtained with synthetic L10-FeNi.

摘要

为了理解L10型有序FeNi合金的硬磁性,我们从天然陨石中提取了L10-FeNi相,并评估了其基本的固态性质:样品成分、磁滞、晶体结构和电子结构。我们使用配备电子探针微分析仪的扫描电子显微镜(SEM-EPMA)、超导量子干涉仪(SQUID)、X射线衍射(XRD)和磁圆二色性(MCD)进行了多方向分析。结果,我们发现其成分为Fe:50.47±1.98原子百分比,Ni:49.60±1.49原子百分比,并且确认了一个明显的超晶格峰。估计的有序度为0.608,晶格常数a = b = 3.582 Å,c = 3.607 Å。获得的矫顽力超过500 Oe。使用K吸收边的MCD分析表明,磁各向异性可能源于Fe中3d电子的轨道磁矩;该结果与先前使用合成L10-FeNi获得的报告结果一致。

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