Anomalous magnetic properties of quasi two-dimensional van der Waals ferromagnet Fe4GeTe2

TL;DR

This study investigates the complex magnetic behavior of Fe4GeTe2, revealing a temperature-dependent phase transition, spin reorientation, and highly anisotropic magnetocaloric effects, indicating a complex magnetic ground state with multiple Fe sites.

Contribution

It provides the first detailed analysis of the temperature and field-dependent magnetic properties and entropy changes in Fe4GeTe2, highlighting its anomalous magnetic behavior and potential for magnetic applications.

Findings

Paramagnetic to ferromagnetic transition at 270 K

Spin reorientation transition around 115 K

Unusual anisotropic magnetic entropy change behavior

Abstract

We have studied the magnetic properties of quasi two-dimensional itinerant ferromagnet Fe$_4$GeTe$_2$ as functions of temperature and magnetic field ($B$) with field parallel to the $ab$-plane ($B\|ab$) and $c$-axis ($B\|c$) of the crystal. This van der Waals compound undergoes a continuous paramagnetic to ferromagnetic phase transition below $T_C$ = 270.0 K and a pronounced spin reorientation transition at around $T_{SR}$ $\sim$ 115 K where the easy axis of magnetization changes its direction from in-plane to out-of-plane. The temperature evolution of magnetization in the FM state is highly anomalous and extremely sensitive to the direction and strength of applied magnetic field. Magnetic entropy change ($\Delta S_M$) has been estimated in the vicinity of $T_C$ and $T_{SR}$. $\Delta S_M$($T$) is found to be almost isotropic around $T_C$ while it shows very unusual behavior and is sensitive to the direction of applied field at low temperature close to $T_{SR}$. For $B\|c$, $\Delta S_M$ is negative and decreases continuously with field and -$\Delta S_M$($T$) shows a broad maximum around $T_{SR}$ similar to that observe at $T_C$. On the other hand, $\Delta S_M$ is positive in the vicinity of $T_{SR}$ below 1.4 T and -$\Delta S_M$($T$) exhibits a peak at $T_{SR}$ which becomes very sharp at high field for $B\|ab$. These results suggest complex nature of the magnetic ground state of Fe$_4$GeTe$_2$, which is possibly due to the presence of multiple inequivalent Fe sites, their ordering and complexity of spin configuration.