Low-field magnetization processes of hexagonal easy-plane altermagnet $α$-MnTe
Sahana Rößler, Victoria Ginga, Marcus Schmidt, Yurii Prots, Helge Rosner, Ulrich Burkhardt, Ulrich K. Rößler, Alexander A. Tsirlin
TL;DR
This work investigates low-field magnetization processes in the hexagonal easy-plane altermagnet α-MnTe. The authors grow high-purity crystals by iodine-assisted chemical vapor transport and characterize their structure and magnetic properties using XRD, EDXS, BSE, magnetization, resistivity, and specific heat measurements, identifying a Néel transition at $T_N \approx 307$ K and a Mn$^{2+}$ spin state $S=5/2$. They observe complex, domain-driven magnetization with a weak ferromagnetic component along $c$ and a low-field anomaly near $\mu_0 H \approx 1$ T, suggesting metastable domain dynamics rather than conventional spin-flop. A phenomenological micromagnetic model incorporating higher-order anisotropic exchange and Dzyaloshinskii-Moriya-like invariants coupling the weak ferromagnetic moment to the Néel vector explains the absence of spin-flop transitions and attributes the irregular magnetization to redistribution of metastable domains, with implications for altermagnet spintronics.
Abstract
Single crystals of $α$-MnTe were synthesized by chemical vapor transport using iodine as the transport reagent. Structural characterization by powder x-ray diffraction confirmed the hexagonal structure (space group P6$_{3}$/mmc). Magnetization $M(T)$ and specific heat $C_p(T)$ measurements revealed an antiferromagnetic phase transition at $T_N \approx307$ K. The magnetic entropy derived from the $C_p(T)$ data is consistent with the $S = 5/2$ spin state of Mn$^{2+}$ ions. Angle- and field-dependent magnetization measurements indicate complex magnetic responses associated with domains, and show an anomaly around 1 T. These features are analyzed using a phenomenological micromagnetic model that includes higher-order anisotropic exchange interactions coupling the weak ferromagnetic component and the antiferromagnetic order parameter. The model captures the generic behavior of magnetic states and demonstrates that the observed uniaxial and unidirectional anisotropies arise from metastable domain configurations and irreversible magnetization processes.
