Magnetic properties of the quasi-XY Shastry-Sutherland magnet Er2Be2SiO7

被引:0
|
作者
Brassington, A. [1 ]
Ma, Q. [2 ]
Sala, G. [3 ]
Kolesnikov, A. I. [2 ]
Taddei, K. M. [2 ]
Wu, Y. [2 ]
Choi, E. S. [4 ,5 ]
Wang, H. [6 ]
Xie, W. [6 ]
Ma, J. [7 ]
Zhou, H. D. [1 ]
Aczel, A. A. [2 ]
机构
[1] Univ Tennessee, Dept Phys & Astron, Knoxville, TN 37996 USA
[2] Oak Ridge Natl Lab, Neutron Scattering Div, Oak Ridge, TN 37831 USA
[3] Oak Ridge Natl Lab, Oak Ridge, TN 37831 USA
[4] Florida State Univ, Natl High Magnet Field Lab, Tallahassee, FL 32310 USA
[5] Florida State Univ, Dept Phys, Tallahassee, FL 32310 USA
[6] Michigan State Univ, Dept Chem, E Lansing, MI 48824 USA
[7] Shanghai Jiao Tong Univ, Key Lab Artificial Struct & Quantum Control, Shenyang Natl Lab Mat Sci, Shanghai 200240, Peoples R China
来源
PHYSICAL REVIEW MATERIALS | 2024年 / 8卷 / 09期
基金
美国国家科学基金会;
关键词
RARE-EARTH TETRABORIDES; DIMER GROUND-STATE; NEUTRON-DIFFRACTION; PHASE-TRANSITIONS; SPIN LIQUIDS; RE; PLATEAUS; FIELD; HEAT; PR;
D O I
10.1103/PhysRevMaterials.8.094001
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Polycrystalline and single-crystal samples of the insulating Shastry-Sutherland compound Er2Be2SiO7 were synthesized via a solid-state reaction and the floating zone method, respectively. The crystal structure, Er single-ion anisotropy, zero-field magnetic ground state, and magnetic phase diagrams along high-symmetry crystallographic directions were investigated with bulk measurement techniques, x-ray and neutron diffraction, and neutron spectroscopy. We establish that Er2Be2SiO7 crystallizes in a tetragonal space group with planes of orthogonal Er dimers and a strong preference for the Er moments to lie in the local plane perpendicular to each dimer bond. We also find that this system has a noncollinear ordered ground state in zero field with a transition temperature of 0.841 K consisting of antiferromagnetic dimers and in-plane moments. Finally, we mapped out the H-T phase diagrams for Er2Be2SiO7 along the directions H [001], [100], and [110]. While an increasing in-plane field simply induces a phase transition to a field-polarized phase, we identify three metamagnetic transitions in the H [001] case. Single-crystal neutron diffraction results reveal that the H [001] phase diagram can be explained predominantly by the expected field-induced behavior of classical, anisotropic moments, although the microscopic origin of one phase requires further investigation.
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收藏
页数:15
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