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钕铁铬氧化物(NdFeCrO)中稀土和过渡金属亚晶格的负磁化和磁有序

Negative magnetization and magnetic ordering of rare earth and transition metal sublattices in NdFeCrO.

作者信息

Kanthal S, Banerjee A, Chatterjee S, Yanda P, Sundaresan A, Khalyavin D D, Orlandi F, Saha-Dasgupta T, Bandyopadhyay S

机构信息

Department of Physics, University of Calcutta, 92 A.P.C. Road, Kolkata 700009, India.

CRNN, University of Calcutta, Sector III, Salt Lake, Kolkata 700106, India.

出版信息

J Phys Condens Matter. 2024 Jun 11;36(36). doi: 10.1088/1361-648X/ad512b.

Abstract

We investigate the effect of alloying at the 3transition metal site of a rare-earth-transition metal oxide, by considering NdFeCrOmixed perovskite with two equal and random distribution of 3d ions, Cr and Fe, interacting with an early 4f rare earth ion, Nd. Employing temperature- and field- dependent magnetization measurements, temperature-dependent x-ray diffraction, neutron powder diffraction, and Raman spectroscopy, we characterize its structural and magnetic properties. Our study reveals bipolar magnetic switching (arising from negative magnetization) and magnetocaloric effect which underline the potential of the studied mixed perovskite in device application. The neutron diffraction study shows the absence of spin reorientation transition over the entire temperature range of 1.5-320 K, although both parent compounds exhibit spin orientation transition. We discuss the microscopic origin of this curious behavior. The neutron diffraction results also reveal the ordering of Nd spins at an unusually high temperature of about 40 K, which is corroborated by Raman measurements.

摘要

我们通过研究具有3d离子Cr和Fe两种等量且随机分布、并与早期4f稀土离子Nd相互作用的NdFeCrO混合钙钛矿,来探究在稀土过渡金属氧化物的3价过渡金属位点进行合金化的影响。通过依赖温度和磁场的磁化测量、依赖温度的x射线衍射、中子粉末衍射和拉曼光谱,我们对其结构和磁性进行了表征。我们的研究揭示了双极磁开关(由负磁化产生)和磁热效应,这凸显了所研究的混合钙钛矿在器件应用中的潜力。中子衍射研究表明,在1.5 - 320 K的整个温度范围内不存在自旋重取向转变,尽管两种母体化合物都表现出自旋取向转变。我们讨论了这种奇特行为的微观起源。中子衍射结果还揭示了Nd自旋在约40 K的异常高温下的有序排列,这得到了拉曼测量的证实。

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