Cubic magnetic anisotropy in $B$20 magnets: Interplay of anisotropy and magnetic order in Fe$_{1-x}$Co$_{x}$Si
G. Gödecke, A. O. Leonov, J. Grefe, S. Süllow, D. Menzel
TL;DR
The paper investigates cubic magnetocrystalline anisotropy in cubic B20 magnets MnSi and Fe$_{1-x}$Co$_x$Si using angle-resolved SQUID magnetization to extract the fourth-order anisotropy constant $K_1$ via a cubic energy expansion $E_{cub}(\ound) = K_0 + K_1(m_1^2m_2^2 + m_2^2m_3^2 + m_1^2m_3^2)$. It demonstrates a strong concentration dependence of $K_1$ in Fe$_{1-x}$Co$_x$Si, with MnSi having $K_1<0$ ($\langle111\rangle$ easy axes) and Fe-rich compositions showing $K_1>0$ ($\langle100\rangle$ easy axes), including a vanishing anisotropy near $x\approx0.5$ and weaker anisotropy at high $x$; crucially, $x\approx0.08$–$0.15$ yields a unitless anisotropy $k_c$ above a theoretical threshold ($k_c=0.039$), indicating potential stabilization of a low-temperature skyrmion phase (LTS). The study cross-validates $K_1$ through a secondary analysis based on $H_{c2}$ and Dzyaloshinskii-model simulations using $\Delta=(H_{c2[111]}-H_{c2[100]})/H_{c2[100]}$, finding broad agreement and identifying Fe$_{1-x}$Co$_x$Si concentrations most favorable for LTS engineering. Altogether, the work provides a quantitative anisotropy map for Fe$_{1-x}$Co$_x$Si and MnSi, clarifying how weak cubic anisotropy interacts with magnetic order and supports anisotropy-driven skyrmion stabilization in itinerant chiral magnets.
Abstract
The metallic systems MnSi and Fe$_{1-x}$Co$_{x}$Si 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 Cu$_2$OSeO$_3$ 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 Fe$_{1-x}$Co$_{x}$Si ($0.08 \leq x \leq 0.70$) single crystals and provide quantitative values of the anisotropy constants. For Fe$_{1-x}$Co$_{x}$Si, the cubic anisotropy is found to be strongly dependent on the Co concentration $x$. In particular, for low Co concentrations ($x \sim 0.10$), the anisotropy is sufficiently strong to stabilize a low-temperature skyrmion lattice, in agreement with theoretical predictions. This finding suggests that Fe$_{1-x}$Co$_{x}$Si 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.
