Abstract
The quasi-two-dimensional Shastry-Sutherland model has remained topical in the field of condensed matter physics for the last two decades, following the experimental realization of the model in the material SrCu2(BO3)2. Since then, research into the Shastry-Sutherland system has revealed more nuanced physics than initially predicted; recent theoretical works have even predicted a quantum spin liquid phase may exist. Herein, we report on a new Shastry-Sutherland lattice material, Yb2Be2GeO7, of the rare-earth melilite family RE2Be2GeO7. We find, through SQUID magnetometry, powder neutron diffraction, specific heat capacity, and muon spin relaxation, that Yb2Be2GeO7 lacks magnetic order and exhibits persistent spin dynamics to at least 17 mK. We propose the Shastry-Sutherland lattice material Yb2Be2GeO7 as a candidate to host a quantum spin liquid ground state.
| Original language | English |
|---|---|
| Article number | 014412 |
| Journal | Physical Review B |
| Volume | 110 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jul 1 2024 |
Funding
We thank Dr. Bruce Gaulin and Dr. Jeff Rau for their helpful discussions. Work at McMaster University was supported by the Natural Sciences and Engineering Research Council of Canada. A portion of this research used resources at the High Flux Isotope Reactor, a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. Work at the University of Birmingham was supported by the UKRI Engineering and Physical Sciences Research Council (EP/V028774/1). The authors also acknowledge support from the University of Birmingham and McMaster University through the BIRMAC Quantum Materials Fund. We thank Dr. Bruce Gaulin and Dr. Jeff Rau for their helpful discussions. Work at McMaster University was supported by the Natural Sciences and Engineering Research Council of Canada. A portion of this research used resources at the High Flux Isotope Reactor, a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. Work at the University of Birmingham was supported by the UKRI Engineering and Physical Sciences Research Council (EP/V028774/1). The authors also acknowledge support from the University of Birmingham and McMaster University through the BIRMAC Quantum Materials Fund. We thank Dr. Bruce Gaulin and Dr. Jeff Rau for their helpful discussions. Work at McMaster University was supported by the Natural Sciences and Engineering Research Council of Canada. A portion of this research used resources at the High Flux Isotope Reactor, a DOE Office of Science User Facility operated by the Oak Ridge National Laboratory. Work at the University of Birmingham was supported by the UKRI Engineering and Physical Sciences Research Council (EP/V028774/1). The authors also acknowledge support from the University of Birmingham and McMaster University through the BIRMAC Quantum Materials Fund
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