Role of magnetic anisotropy in the antiskyrmion-host schreibersite magnets

被引:0
|
作者
Hemmida, M. [1 ]
Masell, J. [2 ,3 ]
Karube, K. [3 ]
Ehlers, D. [1 ]
von Nidda, H. -A. Krug [1 ]
Tsurkan, V. [1 ,4 ]
Tokura, Y. [3 ,5 ,6 ,7 ]
Taguchi, Y. [3 ]
Kezsmarki, I. [1 ]
机构
[1] Univ Augsburg, Ctr Elect Correlat & Magnetism, Expt Phys 5, D-86135 Augsburg, Germany
[2] Karlsruhe Inst Technol KIT, Inst Theoret Solid State Phys, D-76049 Karlsruhe, Germany
[3] RIKEN Ctr Emergent Matter Sci CEMS, Wako 3510198, Japan
[4] Moldova State Univ, Inst Appl Phys, MD-2028 Kishinev, Moldova
[5] Univ Tokyo, Dept Appl Phys, Tokyo 1138656, Japan
[6] Univ Tokyo, Quantum Phase Elect Ctr QPEC, Tokyo 1138656, Japan
[7] Univ Tokyo, Tokyo Coll, Tokyo 1138656, Japan
关键词
SKYRMION LATTICE; TEMPERATURE; CRYSTALS;
D O I
10.1103/PhysRevB.110.054416
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Magnetic anisotropy is a fundamental property of magnetic materials that plays an essential role in the stability of magnetic domains and skyrmions. In this ferromagnetic resonance study, we report the evolution of magnetic anisotropy by substituting various 4d metals in the antiskyrmion host (Fe, Ni)3P with S4 tetragonal symmetry. In the undoped compound (Fe0.63Ni0.37)3P and in the Ru-doped (Fe0.59Ni0.32Ru0.09)3P, the uniaxial magnetic anisotropy has an easy-plane character, while Pd doping turns the material to an easy-axis-type magnet, as observed in (Fe0.62Ni0.29Pd0.09)3P. In addition to the dominant uniaxial anisotropy, we also quantify the fourfold anisotropy of the plane perpendicular to the tetragonal axis in (Fe0.63Ni0.30Pd0.07)3P. Using analytical calculations and micromagnetic simulations, we discuss how this planar anisotropy competes with the anisotropic Dzyaloshinskii-Moriya interaction in determining the orientation of the magnetic stripes and the antiskyrmions.
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页数:10
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