Magnetic structure, excitations, and field-induced transitions in the honeycomb lattice compound Er2Si2O7

被引:0
|
作者
Islam, M. [1 ]
d'Ambrumenil, N. [1 ]
Khalyavin, D. D. [2 ]
Manuel, P. [2 ]
Orlandi, F. [2 ]
Ollivier, J. [3 ]
Hatnean, M. Ciomaga [1 ,4 ,5 ]
Balakrishnan, G. [1 ]
Petrenko, O. A. [1 ]
机构
[1] Univ Warwick, Dept Phys, Coventry CV4 7AL, England
[2] STFC Rutherford Appleton Lab, ISIS Facil, Didcot OX11 0QX, England
[3] Inst Laue Langevin, 71 Ave Martyrs,CS 20156, F-38042 Grenoble 9, France
[4] Swiss Fed Inst Technol, Dept Mat, Mat Discovery Lab, CH-8093 Zurich, Switzerland
[5] Paul Scherrer Inst PSI, Lab Multiscale Mat Expt, CH-5232 Villigen, Switzerland
基金
英国工程与自然科学研究理事会;
关键词
RARE-EARTH DISILICATES; GROWTH;
D O I
10.1103/PhysRevB.109.094420
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We investigate the magnetic properties of the monoclinic D-type Er2Si2O7 with a distorted honeycomb lattice using powder and single-crystal neutron scattering techniques, as well as single-crystal magnetization measurements. The powder neutron diffraction shows that below the ordering temperature, TN = 1.85 K, the compound forms a q = 0 antiferromagnetic structure with four sublattices. For H II a, magnetization measurements reveal a narrow but clearly visible plateau at one-third of the magnetization saturation value. The plateau's stabilization is accompanied by a significant increase of the magnetic unit cell, as the magnetic peaks with fractional indices are observed in single-crystal neutron diffraction experiments. At low temperatures, the inelastic neutron scattering measurements reveal the presence of low-energy, almost dispersionless excitations. Their spectrum is sensitive to the applied field, it significantly softens on the magnetization plateau, and demonstrates the behavior expected for a noncollinear Ising antiferromagnet away from the plateau.
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页数:11
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