Magnetic Behavior of Volborthite Cu3V2O7(OH)2•2H2O Determined by Coupled Trimers Rather than Frustrated Chains

被引:48
|
作者
Janson, O. [1 ]
Furukawa, S. [2 ]
Momoi, T. [3 ,4 ]
Sindzingre, P. [5 ]
Richter, J. [6 ]
Held, K. [1 ]
机构
[1] TU Wien, Inst Festkorperphys, Wiedner Hauptstr 8-10, A-1040 Vienna, Austria
[2] Univ Tokyo, Dept Phys, Bunkyo Ku, 7-3-1 Hongo, Tokyo 1130033, Japan
[3] RIKEN, Condensed Matter Theory Lab, Wako, Saitama 3510198, Japan
[4] RIKEN, CEMS, Wako, Saitama 3510198, Japan
[5] Univ Paris 06, Lab Phys Theor Mat Condensee, F-75252 Paris, France
[6] Univ Magdeburg, Inst Theoret Phys, D-39016 Magdeburg, Germany
基金
欧洲研究理事会;
关键词
LIQUID GROUND-STATE; KAGOME; KAPELLASITE; FIELD;
D O I
10.1103/PhysRevLett.117.037206
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Motivated by recent experiments on volborthite single crystals showing a wide 1/3-magnetization plateau, we perform microscopic modeling by means of density functional theory (DFT) with the single-crystal structural data as a starting point. Using DFT + U, we find four leading magnetic exchanges: antiferromagnetic J and J(2), as well as ferromagnetic J' and J(1). Simulations of the derived spin Hamiltonian show good agreement with the experimental low-field magnetic susceptibility and high-field magnetization data. The 1/3-plateau phase pertains to polarized magnetic trimers formed by strong J bonds. An effective J. 8 model shows a tendency towards condensation of magnon bound states preceding the plateau phase.
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收藏
页数:6
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