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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.

Cubic magnetic anisotropy in $B$20 magnets: Interplay of anisotropy and magnetic order in Fe$_{1-x}$Co$_{x}$Si

TL;DR

The paper investigates cubic magnetocrystalline anisotropy in cubic B20 magnets MnSi and FeCoSi using angle-resolved SQUID magnetization to extract the fourth-order anisotropy constant via a cubic energy expansion . It demonstrates a strong concentration dependence of in FeCoSi, with MnSi having ( easy axes) and Fe-rich compositions showing ( easy axes), including a vanishing anisotropy near and weaker anisotropy at high ; crucially, yields a unitless anisotropy above a theoretical threshold (), indicating potential stabilization of a low-temperature skyrmion phase (LTS). The study cross-validates through a secondary analysis based on and Dzyaloshinskii-model simulations using , finding broad agreement and identifying FeCoSi concentrations most favorable for LTS engineering. Altogether, the work provides a quantitative anisotropy map for FeCoSi 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 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.

Paper Structure

This paper contains 8 sections, 4 equations, 8 figures.

Figures (8)

  • Figure 1: Schematic depiction of the phase diagram of Fe$_{1-x}$Co$_{x}$Si as function of the Co concentration $x$. At low Co concentrations, Fe$_{1-x}$Co$_{x}$Si undergoes an insulator-to-metal transition, closely followed by a nonmagnetic-to-magnetic transition Grefe2024. For Co concentrations up to $x=0.50$, a high-temperature skyrmion phase (HTS) persists near $T_\text{HM}$grigoriev2007grigoriev2007_principal_interactionsmuenzer_2010bauer2016_history with a strong history dependence bauer2016_history as indicated by arrows. At high Co concentrations near $x\approx 0.65$ Fe$_{1-x}$Co$_{x}$Si shows a tendency to show full field polarization (FP) Grigoriev2022_FM. From studies on Cu$_2$OSeO$_3$2018Chacon2018Halder, the question arises whether the tunable system Fe$_{1-x}$Co$_{x}$Si also features a low-temperature skyrmion phase (LTS).
  • Figure 2: (a) Rotatable sample holder used to conduct angle-resolved magnetization measurements and (b) exemplary measurements of the magnetic moment upon sample rotation for Fe$_{0.92}$Co$_{0.08}$Si at $T=5~\text{K}$. The magnetization direction relative to the crystal orientation is parameterized by the angles $\theta$ and $\phi$.
  • Figure 3: Magnetization energies $E$ as a function of the crystal orientation at $T=5~\text{K}$ for (a) MnSi with $\phi=45^\circ$, (b) Fe$_{0.92}$Co$_{0.08}$Si with $\phi=45^\circ$, (c) Fe$_{0.50}$Co$_{0.50}$Si with $\phi=0^\circ$ and (d) Fe$_{0.35}$Co$_{0.65}$Si with $\phi=45^\circ$. Red lines represent the cubic anisotropy fit according to Eq. (\ref{['eq:cubic_anisotropy']}). (a) represents the case of $K_1<0$, (b) and (d) the case of $K_1>0$, and (c) $K_1=0$ within the resolution of our experiment.
  • Figure 4: Anisotropy constants $-K_1$ for MnSi and $K_1$ for Fe$_{1-x}$Co$_{x}$Si ($0.08 \leq x \leq 0.70$) at $T=5~\text{K}$ and $T=10~\text{K}$. Dashed lines are guides to the eye.
  • Figure 5: Magnetization $M$ for Fe$_{0.85}$Co$_{0.15}$Si at $T=5~\text{K}$ along the $\langle 100 \rangle$ and $\langle 111\rangle$ directions. The red-shaded region marks the area contributing with an opposite sign to the magnetic anisotropy. The critical fields are obtained from the first derivative and through linear interpolations near saturation.
  • ...and 3 more figures