Probing magnetoelectric effect in the spin-modulated magnet Fe2GeO4

The distinct spin amplitude wave was reported in a highly frustrated magnetic compound Fe2GeO4, which is very different from observations on other members of the M2GeO4 (M = Fe, Co, and Ni) family, raising interest in this compound for some additional emergent phenomena. In particular, this non-uniform spin order allows the intrinsic connection between ferroelectric polarization and magnetically gradient structure to probe the potential linear magnetoelectric (ME) effect. In this work, we address this issue and investigate the magnetism of Fe2GeO4 single crystal that hosts two successive anomalies at antiferromagnetic (AFM) Neel temperatures T (N1) similar to 7.5 K and T (N2) similar to 6.7 K, respectively. Our results reveal a remarkable metamagnetic transition in the magnetization as a function of the magnetic field, occurring at a critical magnetic field H (c) similar to 4.1 T when applied along the [110] and [1-10] directions, while such transition along the [001] direction is pointedly absent. Further exploration uncovers two predominant off-diagonal ME coefficients alpha(yz) and alpha(zy) in the incommensurate AFM phase between T (N1) and T (N2). Additionally, all components of the linear ME tensor remain non-vanishing in the canting AFM phase below T (N2). This indicates the ME mechanisms for the two phases that may be driven by different magnetic structures. All these presented results are sufficient for us to draw a non-trivial ME phase diagram, which is beneficial to understanding the ME behavior of Fe2GeO4. Therefore, our study implies that Fe2GeO4, an unusual frustrated magnet, provides a platform for manipulating the fascinating ME effect in the spinel structure.

Automated summary

A distinct spin amplitude wave is discovered in the highly frustrated magnetic compound Fe2GeO4, which differs from observations in other members of the M2GeO4 family, sparking interest in additional emergent phenomena. The non-uniform spin order in Fe2GeO4 allows for the exploration of the intrinsic connection between ferroelectric polarization and magnetically gradient structure to probe potential linear magnetoelectric effects.