Rozova M G, Grigoriev V V, Bobrikov I A, Filimonov D S, Zakharov K V, Volkova O S, Vasiliev A N, Antipov E V, Tsirlin A A, Abakumov A M
Department of Chemistry, Moscow State University, 119991 Moscow, Russia.
Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, 6 Joliot-Curie Street, 141980 Dubna, Russia.
Dalton Trans. 2016 Jan 21;45(3):1192-200. doi: 10.1039/c5dt04296h.
Highly homogeneous mullite-type solid solutions Bi2Fe(4-x)CrxO9 (x = 0.5, 1, 1.2) were synthesized using a soft chemistry technique followed by a solid-state reaction in Ar. The crystal structure of Bi2Fe3CrO9 was investigated using X-ray and neutron powder diffraction, transmission electron microscopy and (57)Fe Mössbauer spectroscopy (S.G. Pbam, a = 7.95579(9) Å, b = 8.39145(9) Å, c = 5.98242(7) Å, RF(X-ray) = 0.022, RF(neutron) = 0.057). The ab planes in the structure are tessellated with distorted pentagonal loops built up by three tetrahedrally coordinated Fe sites and two octahedrally coordinated Fe/Cr sites, linked together in the ab plane by corner-sharing forming a pentagonal Cairo lattice. Magnetic susceptibility measurements and powder neutron diffraction show that the compounds order antiferromagnetically (AFM) with the Néel temperatures decreasing upon increasing the Cr content from TN ∼ 250 K for x = 0 to TN ∼ 155 K for x = 1.2. The magnetic structure of Bi2Fe3CrO9 at T = 30 K is characterized by a propagation vector k = (1/2,1/2,1/2). The tetrahedrally coordinated Fe cations form singlet pairs within dimers of corner-sharing tetrahedra, but spins on the neighboring dimers are nearly orthogonal. The octahedrally coordinated (Fe,Cr) cations form antiferromagnetic up-up-down-down chains along c, while the spin arrangement in the ab plane is nearly orthogonal between nearest neighbors and collinear between second neighbors. The resulting magnetic structure is remarkably different from the one in pure Bi2Fe4O9 and features several types of spin correlations even on crystallographically equivalent exchange that may be caused by the simultaneous presence of Fe and Cr on the octahedral site.
采用软化学技术,随后在氩气中进行固态反应,合成了高度均匀的莫来石型固溶体Bi2Fe(4-x)CrxO9(x = 0.5、1、1.2)。使用X射线和中子粉末衍射、透射电子显微镜和(57)Fe穆斯堡尔谱对Bi2Fe3CrO9的晶体结构进行了研究(空间群Pbam,a = 7.95579(9) Å,b = 8.39145(9) Å,c = 5.98242(7) Å,RF(X射线)= 0.022,RF(中子)= 0.057)。该结构中的ab平面由扭曲的五角形环镶嵌而成,这些环由三个四面体配位的Fe位点和两个八面体配位的Fe/Cr位点构成,它们在ab平面中通过角共享连接在一起,形成五角形开罗晶格。磁化率测量和粉末中子衍射表明,这些化合物呈反铁磁有序(AFM),随着Cr含量从x = 0时的TN ∼ 250 K增加到x = 1.2时的TN ∼ 155 K,奈尔温度降低。Bi2Fe3CrO9在T = 30 K时的磁结构由传播矢量k = (1/2,1/2,1/2)表征。四面体配位的Fe阳离子在角共享四面体的二聚体内形成单重态对,但相邻二聚体上的自旋几乎正交。八面体配位的(Fe,Cr)阳离子沿c轴形成反铁磁的上-上-下-下链,而ab平面中的自旋排列在最近邻之间几乎正交,在次近邻之间共线。所得的磁结构与纯Bi2Fe4O9中的显著不同,并即使在晶体学等效交换上也具有几种类型的自旋相关性,这可能是由于八面体位置上同时存在Fe和Cr所致。