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具有长程序磁有序的空位无序、缺氧钙钛矿:Sr2Fe1.5Cr0.5O5 的局域和平均结构及磁性质。

A vacancy-disordered, oxygen-deficient perovskite with long-range magnetic ordering: local and average structures and magnetic properties of Sr2Fe1.5Cr0.5O5.

机构信息

Department of Chemistry, McMaster University, Hamilton, Canada L8S 4M.

出版信息

Inorg Chem. 2012 Feb 20;51(4):2638-44. doi: 10.1021/ic202590r. Epub 2012 Jan 30.

DOI:10.1021/ic202590r
PMID:22288463
Abstract

The local and average crystal structures and magnetic properties of the oxygen-deficient perovskite Sr(2)Fe(1.5)Cr(0.5)O(5+y) were studied using powder X-ray and neutron diffraction, neutron-pair distribution function analysis, and electron energy-loss spectroscopy. This material crystallizes in the cubic Pm3m space group, with a = 3.94491(14) Å. The oxygen vacancies are distributed randomly throughout the perovskite-type structure, and the average coordination number of the Fe(Cr) sites is 5. Refinement of the neutron diffraction data indicates y ∼ 0.05. This is in discordance with an earlier report on a material with the same nominal composition and cell constant. Electron energy-loss Cr L(2,3)-edge spectroscopy shows that Cr(3+) is present, which is also contrary to previous speculation. Neutron-pair distribution function studies show that a brownmillerite-like model involving ordered vacancies and alternating octahedral and tetrahedral coordination at the metal sites, gives a better description of the local structure out to ∼5 Å. A remarkable phenomenon determined by neutron diffraction in Sr(2)Fe(1.5)Cr(0.5)O(5) is the occurrence of a long-range G-type antiferromagnetic ordering with T(c) ≈ 565 K because cubic oxygen-deficient perovskites with B-site disorder usually do not undergo transitions to magnetically ordered states. The observation of long-range antiferromagnetic order and the T(c) value are in accordance with previous Mössbauer spectroscopic studies.

摘要

采用粉末 X 射线和中子衍射、中子对分布函数分析和电子能量损失光谱研究了氧空位钙钛矿 Sr(2)Fe(1.5)Cr(0.5)O(5+y)的局域和平均晶体结构和磁性能。该材料在立方 Pm3m 空间群中结晶,a = 3.94491(14)Å。氧空位在钙钛矿型结构中随机分布,Fe(Cr) 位的平均配位数为 5。对中子衍射数据的精修表明 y∼0.05。这与具有相同名义组成和晶胞常数的材料的早期报告不一致。电子能量损失 Cr L(2,3)-边谱表明存在 Cr(3+),这也与之前的推测相矛盾。中子对分布函数研究表明,一种类似于布朗米勒ite 的模型,涉及有序空位和金属位的八面体和四面体配位的交替,对局部结构的描述更好,可达约 5 Å。中子衍射在 Sr(2)Fe(1.5)Cr(0.5)O(5)中确定的一个显著现象是发生长程 G 型反铁磁有序,T(c)≈565 K,因为 B 位无序的立方缺氧钙钛矿通常不会经历向磁有序态的转变。长程反铁磁有序和 T(c)值的观察与之前的穆斯堡尔光谱研究一致。

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