Cubic magnetic anisotropy in 20 magnets: Interplay of anisotropy and magnetic order in FeCoSi
arXiv:2510.09268 · doi:10.1103/h76w-8twm
Abstract
The metallic systems MnSi and FeCoSi are known to feature a generic magnetic phase diagram primarily determined by the isotropic exchange and Dzyaloshinskii-Moriya interactions. However, additional weaker anisotropies, lowest in the hierarchy of energy scales, play a crucial role: they determine the relative order of phases in the phase diagram and may even enable skyrmion stability far below the ordering temperature. Among cubic B20 helimagnets, the insulator CuOSeO is currently the only known example exhibiting a low-temperature, anisotropy-induced skyrmion pocket. In this manuscript, we present a systematic study of cubic magnetocrystalline anisotropy by means of angle-resolved SQUID magnetization measurements in MnSi and FeCoSi () single crystals and provide quantitative values of the anisotropy constants. For FeCoSi, the cubic anisotropy is found to be strongly dependent on the Co concentration . In particular, for low Co concentrations (), the anisotropy is sufficiently strong to stabilize a low-temperature skyrmion lattice, in agreement with theoretical predictions. This finding suggests that FeCoSi may represent the first chiral metallic system to exhibit a low-temperature skyrmion phase controllably stabilized by cubic anisotropy for specific directions of the magnetic field.
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