Ground States of the Ising Model on the Shastry-Sutherland Lattice and the Origin of the Fractional Magnetization Plateaus in Rare-Earth Tetraborides

TL;DR

This paper provides an exact solution for the ground states of the Ising model on the Shastry-Sutherland lattice, clarifying the origin of fractional magnetization plateaus in rare-earth tetraborides and predicting new plateaus with extended interactions.

Contribution

It offers the first complete ground-state solution for the Ising model on this lattice and explains the emergence of observed and potential magnetization plateaus in RB4 compounds.

Findings

The 1/3 magnetization plateau is the only fractional plateau in the basic model.

Stripe magnetic structures with 1/2 and 1/n magnetization occur at phase boundaries.

Longer-range interactions can induce additional plateaus, such as the 1/2 plateau.

Abstract

A complete and exact solution of the ground-state problem for the Ising model on the Shastry-Sutherland lattice in the applied magnetic field is found. The magnetization plateau at the one third of the saturation value is shown to be the only possible fractional plateau in this model. However, stripe magnetic structures with magnetization 1/2 and $1/n$ ($n > 3$), observed in the rare-earth tetraborides RB$_4$, occur at the boundaries of the three-dimensional regions of the ground-state phase diagram. These structures give rise to new magnetization plateaus if interactions of longer ranges are taken into account. For instance, an additional third-neighbor interaction is shown to produce a 1/2 plateau. The results obtained significantly refine the understanding of the magnetization process in RB$_4$ compounds, especially in TmB$_4$ and ErB$_4$ which are strong Ising magnets.