Magnetic order in the rare-earth ferroborate CeFe3(BO3)4

被引:5
|
作者
Hayashida, Shohei [1 ]
Asai, Shinichiro [1 ]
Kato, Daiki [1 ]
Hasegawa, Shunsuke [1 ]
Avdeev, Maxim [2 ,3 ]
Cao, Huibo [4 ]
Masuda, Takatsugu [1 ]
机构
[1] Univ Tokyo, Inst Solid State Phys, Chiba 2778581, Japan
[2] Australian Nucl Sci & Technol Org, Menai, NSW 2234, Australia
[3] Univ Sydney, Sch Chem, Sydney, NSW 2006, Australia
[4] Oak Ridge Natl Lab, Neutron Scattering Div, Oak Ridge, TN 37831 USA
基金
日本学术振兴会;
关键词
Rare earths - Iron compounds - Single crystals - Cerium compounds - Magnetic susceptibility - Neutrons - Neutron diffraction - Crystallography - Antiferromagnetism - Phase separation - Magnetic moments - Magnetic structure;
D O I
10.1103/PhysRevB.98.224405
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We have studied the magnetic order of the rare-earth ferroborate CeFe3(BO3)(4) through the thermodynamic and the neutron diffraction measurements. The heat capacity and the magnetic susceptibility revealed antiferromagnetic magnetic ordering at 29 K. In the neutron powder diffraction data, we observed the magnetic Bragg peaks indexed by the commensurate (CM) propagation vector k(CM) = (0, 0, 3/2) and the incommensurate (ICM) vector k(ICM) = (0, 0, 3/2+delta). The incommensurability delta increases with decreasing the temperature, and is evaluated to be 0.04556(16) at 3.7 K. Magnetic structure analysis reveals that the magnetic moments aligning in the ab plane form the collinear antiferromagnetic structure having k(CM)( )and helical structure having k(ICM). Detailed measurements of the magnetic susceptibility exhibit an additional anomaly at 27 K. Furthermore, the temperature dependence of the neutron diffraction profile on the single-crystal sample shows that the ICM and CM ordering occurs at 29 and 26 K, respectively. These results suggest a phase separation state between the collinear and helical structures. The multiferroicity of CeFe3(BO3)(4) is discussed on the basis of the determined magnetic structure.
引用
收藏
页数:9
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