Disentangling the unusual magnetic anisotropy of the near-room-temperature ferromagnet Fe$_{4}$GeTe$_{2}$
Riju Pal, Joyal J. Abraham, Alexander Mistonov, Swarnamayee Mishra, Nina Stilkerich, Suchanda Mondal, Prabhat Mandal, Atindra Nath Pal, Jochen Geck, Bernd Büchner, Vladislav Kataev, Alexey Alfonsov
TL;DR
This work uses high-field electron spin resonance to dissect the unusual magnetic anisotropy in Fe$_{4}$GeTe$_{2}$, a near-room-temperature ferromagnet with layered, quasi-2D character. By analyzing frequency- and temperature-dependent resonance fields, the authors separate shape (demagnetization) and intrinsic magnetocrystalline contributions to the total anisotropy, revealing a dominant shape component above $T_ ext{shape}\approx 150$ K and an intrinsic easy-axis anisotropy that grows at lower temperatures, with a crossover near $T_ ext{cross}\approx 110$ K and further complexity below $T_ ext{d}\approx 50$ K. X-ray diffraction shows no lattice transition but uncovers a robust in-plane superlattice, indicating the spin reorientation is mainly magnetoelastic and electronic in origin rather than structural. The characteristic temperatures extracted from ESR align with transport measurements, suggesting a strong magnetoelectronic coupling and indicating that the observed low-dimensional magnetism persists toward monolayer behavior, which is promising for spintronic applications. The findings provide a quantitative framework for tuning magnetic and electronic properties via anisotropy management in this material system.
Abstract
In the quest for two-dimensional conducting materials with high ferromagnetic ordering temperature the new family of the layered Fe$_{n}$GeTe$_{2}$ compounds, especially the near-room-temperature ferromagnet Fe$_{4}$GeTe$_{2}$, receives a significant attention. Fe$_{4}$GeTe$_{2}$ features a peculiar spin reorientation transition at $T_\mathrm{SR} \sim 110$ K suggesting a non-trivial temperature evolution of the magnetic anisotropy (MA) - one of the main contributors to the stabilization of the magnetic order in the low-D systems. An electron spin resonance (ESR) spectroscopic study reported here provides quantitative insights into the unusual magnetic anisotropy of Fe$_{4}$GeTe$_{2}$. At high temperatures the total MA is mostly given by the demagnetization effect with a small contribution of the counteracting intrinsic magnetic anisotropy of an easy-axis type, whose growth below a characteristic temperature $T_{\rm shape} \sim 150$ K renders the sample seemingly isotropic at $T_\mathrm{SR}$. Below one further temperature $T_{\rm d} \sim 50$ K the intrinsic MA becomes even more complex. Importantly, all the characteristic temperatures found in the ESR experiment match those observed in transport measurements, suggesting an inherent coupling between magnetic and electronic degrees of freedom in Fe$_{4}$GeTe$_{2}$. This finding together with the observed signatures of the intrinsic two-dimensionality should facilitate optimization routes for the use of Fe$_{4}$GeTe$_{2}$ in the magneto-electronic devices, potentially even in the monolayer limit.
