Synthesis, structure and magnetic ordering of the mullite-type Bi2Fe4-xCrxO9 solid solutions with a frustrated pentagonal Cairo lattice

被引:12
|
作者
Rozova, M. G. [1 ]
Grigoriev, V. V. [1 ]
Bobrikov, I. A. [2 ]
Filimonov, D. S. [1 ]
Zakharov, K. V. [3 ]
Volkova, O. S. [3 ,4 ]
Vasiliev, A. N. [3 ,4 ]
Antipov, E. V. [1 ]
Tsirlin, A. A. [5 ]
Abakumov, A. M. [1 ,6 ,7 ]
机构
[1] Moscow MV Lomonosov State Univ, Dept Chem, Moscow 119991, Russia
[2] Joint Inst Nucl Res, Frank Lab Neutron Phys, Dubna 141980, Russia
[3] Moscow MV Lomonosov State Univ, Dept Phys, Low Temp Phys & Superconduct Dept, Moscow 119991, Russia
[4] Ral Fed Univ, Theoret Phys & Appl Math Dept, Ekaterinburg 620002, Russia
[5] Univ Augsburg, Inst Phys, Ctr Elect Correlat & Magnetism, Expt Phys 6, D-86159 Augsburg, Germany
[6] Univ Antwerp, EMAT, B-2020 Antwerp, Belgium
[7] Skolkovo Inst Sci & Technol, Moscow 143025, Russia
基金
俄罗斯科学基金会;
关键词
BI2FE4O9;
D O I
10.1039/c5dt04296h
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
Highly homogeneous mullite-type solid solutions Bi2Fe4-xCrxO9 (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 Fe-57 Mossbauer spectroscopy (S.G. Pbam, a = 7.95579(9) angstrom , b = 8.39145(9) angstrom, c = 5.98242(7) angstrom, R-F(X-ray) = 0.022, R-F(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 Neel temperatures decreasing upon increasing the Cr content from T-N similar to 250 K for x = 0 to T-N similar to 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.
引用
收藏
页码:1192 / 1200
页数:9
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