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通过高角分辨率同步辐射X射线衍射研究EuNiO和GdNiO钙钛矿绝缘态中缺乏单斜畸变:与YNiO的比较

On the lack of monoclinic distortion in the insulating regime of EuNiO and GdNiO perovskites by high-angular resolution synchrotron X-ray diffraction: a comparison with YNiO.

作者信息

Serrano-Sánchez Federico, Martínez José Luis, Fauth François, Alonso José Antonio

机构信息

Instituto de Ciencia de Materiales de Madrid (ICMM), Consejo Superior de Investigaciones Científicas (CSIC), Sor Juana Inés de la Cruz 3, E-28049, Madrid, Spain.

CELLS-ALBA Synchrotron, Cerdanyola del Valles, Barcelona, E-08290, Spain.

出版信息

Dalton Trans. 2021 May 25;50(20):7085-7093. doi: 10.1039/d1dt00646k.

Abstract

Rare-earth nickelates RNiO3 (R = Y, LaLu) are electron-correlated perovskite materials where the interplay between charge and spin order results in a rich phase diagram, evolving from antiferromagnetic insulators to paramagnetic metals. They are well-known to undergo metal-insulator (MI) transitions as a function of temperature and the size of the rare-earth ion. For intermediate-size Eu3+ and Gd3+ ions, the MI transitions are described to happen at TMI = 463 K and 511 K, respectively. We have investigated their structural evolution across TMI with the excellent angular resolution of synchrotron X-ray diffraction, using high-crystalline quality samples prepared at elevated hydrostatic pressures. Unlike YNiO3, synthesized and measured under the same conditions, exhibiting a characteristic monoclinic phase (space group P21/n) in the insulating regime (below TMI), the present EuNiO3 and GdNiO3 samples do not exhibit such a symmetry, but their crystal structures can be defined in an orthorhombic superstructure of perovskite (space group Pbnm) in all the temperature interval, between 100 and 623 K for Eu and 298 K and 650 K for Gd. Nevertheless, an abrupt evolution of the unit-cell parameters is observed upon metallization above TMI. A prior report of a charge disproportionation effect by Mössbauer spectroscopy on Fe-doped perovskite samples seems to suggest that the distribution of two distinct Ni sites must not exhibit the required long-range ordering to be effectively detected by diffraction methods. An abrupt contraction of the b parameter of EuNiO3 in the 175-200 K range, coincident with the onset of antiferromagnetic ordering, suggests a magnetoelastic coupling, not described so far in rare-earth nickelates. The magnetic susceptibility is dominated by the paramagnetic signal of the rare-earth ions; however, the AC susceptibility curves yield a Néel temperature corresponding to the antiferromagnetic ordering of the Ni moments of TN = 197 K for EuNiO3, corroborated by specific heat measurements. For GdNiO3, a χT vs. T plot presents a clear change in the slope at TN = 187 K, also consistent with specific heat data. Magnetization measurements at 2 K under large fields up to 14 T show a complete saturation of the magnetic moments with a rather high ordered moment of 7.5μB per f.u.

摘要

稀土镍酸盐RNiO₃(R = Y、La、Lu)是电子关联的钙钛矿材料,其中电荷与自旋序之间的相互作用导致了丰富的相图,从反铁磁绝缘体演变为顺磁金属。众所周知,它们会随着温度和稀土离子尺寸的变化发生金属-绝缘体(MI)转变。对于中等尺寸的Eu³⁺和Gd³⁺离子,MI转变分别发生在TMI = 463 K和511 K。我们使用在高压下制备的高结晶质量样品,通过同步加速器X射线衍射的出色角分辨率研究了它们在TMI附近的结构演变。与在相同条件下合成和测量的YNiO₃不同,YNiO₃在绝缘状态(低于TMI)下呈现出特征性的单斜相(空间群P21/n),而目前的EuNiO₃和GdNiO₃样品并未表现出这种对称性,但它们的晶体结构可以在钙钛矿的正交超结构(空间群Pbnm)中定义,在整个温度区间内,Eu的温度范围是100至623 K,Gd的温度范围是298至650 K。然而,在高于TMI的金属化过程中观察到晶胞参数的突然变化。先前一篇关于穆斯堡尔光谱对铁掺杂钙钛矿样品电荷 disproportionation 效应的报告似乎表明,两个不同Ni位点的分布不一定表现出通过衍射方法有效检测所需的长程有序。EuNiO₃的b参数在175 - 200 K范围内突然收缩,这与反铁磁有序的开始同时发生,表明存在磁弹性耦合,这在稀土镍酸盐中尚未有过描述。磁化率主要由稀土离子的顺磁信号主导;然而,交流磁化率曲线给出了对应于EuNiO₃中Ni磁矩反铁磁有序的奈尔温度TN = 197 K,这得到了比热测量的证实。对于GdNiO₃,χT对T的曲线在TN = 187 K处斜率有明显变化,这也与比热数据一致。在高达14 T的大磁场下2 K时的磁化测量表明,磁矩完全饱和,每个f.u.具有相当高的有序磁矩7.5μB 。

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