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PrFeCrO:一种I型多铁性材料。

PrFeCrO: A Type I Multiferroic.

作者信息

Das Nibedita, Singh Satyendra, Joshi Amish G, Thirumal Meganathan, Reddy V Raghavendra, Gupta Laxmi Chand, Ganguli Ashok Kumar

机构信息

Department of Chemistry, Indian Institute of Technology Delhi , Hauz Khas, New Delhi 110016, India.

Centre for Nano Science, Jawaharlal Nehru University , New Delhi 110067, India.

出版信息

Inorg Chem. 2017 Nov 6;56(21):12712-12718. doi: 10.1021/acs.inorgchem.7b01086. Epub 2017 Oct 6.

DOI:10.1021/acs.inorgchem.7b01086
PMID:28984458
Abstract

We synthesized double perovskite PrFeCrO by solid-state method. Analysis of its X-ray powder diffraction shows that the compound crystallizes in a centrosymmetric structure with space group Pbnm. Our X-ray photoelectron spectroscopy (XPS) studies show that all the cations are present in +3 oxidation state. Magnetization studies of PrFeCrO show that the material is paramagnetic at room temperature and undergoes a magnetic transition below T = 250 K. We observe clear magnetic hysteresis loop, for example, below 150 K. A low remnant magnetization M, ∼0.05 μ/f. u., is inferred from the observed magnetic hysteresis loop. Fe Mössbauer study at 25 K shows a high hyperfine magnetic field of ∼53 T at the Fe nucleus, which corresponds to a magnetic moment of ∼6-7 μ/Fe. These two results together suggest a ferrimagnetic (nearly compensated or canted) ordering of the Fe moments. Mössbauer studies close to the ferrimagnetic ordering temperature suggest interesting magnetic relaxation effects. A dielectric anomaly observed at T = 453 K signals a ferroelectric ↔ paraelectric phase transition. We observe at room temperature a clear and well-defined ferroelectric hysteresis loop, P = 1.04 μC/cm, establishing ferroelectricity in the material. From these results, we conclude that PrFeCrO is a type I multiferroic (T > T).

摘要

我们通过固态法合成了双钙钛矿PrFeCrO。对其X射线粉末衍射的分析表明,该化合物结晶为具有空间群Pbnm的中心对称结构。我们的X射线光电子能谱(XPS)研究表明,所有阳离子均以+3氧化态存在。PrFeCrO的磁化研究表明,该材料在室温下是顺磁性的,并且在T = 250 K以下发生磁转变。例如,在150 K以下我们观察到清晰的磁滞回线。从观察到的磁滞回线推断出低剩余磁化强度M,约为0.05 μ/f.u.。在25 K下的Fe穆斯堡尔研究表明,Fe原子核处的超精细磁场高达约53 T,这对应于约6 - 7 μ/Fe的磁矩。这两个结果共同表明Fe磁矩的亚铁磁性(近乎补偿或倾斜)有序排列。接近亚铁磁性有序温度的穆斯堡尔研究表明存在有趣的磁弛豫效应。在T = 453 K观察到的介电异常表明发生了铁电↔顺电相变。我们在室温下观察到清晰且明确的铁电滞回线,P = 1.04 μC/cm²,证实了该材料中的铁电性。从这些结果,我们得出结论,PrFeCrO是一种I型多铁性材料(T > T)。 (注:原文中最后“T > T”表述有误,可能是遗漏了具体温度数值等信息,但按要求未做修改直接翻译)

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