Abstract
The quantum dimer magnet (QDM) is the canonical example of quantum magnetism. The QDM state consists of entangled nearest-neighbor spin dimers and often exhibits a field-induced triplon Bose-Einstein condensate (BEC) phase. We report on a new QDM in the strongly spin-orbit coupled, distorted honeycomb-lattice material Yb2Si2O7. Our single crystal neutron scattering, specific heat, and ultrasound velocity measurements reveal a gapped singlet ground state at zero field with sharp, dispersive excitations. We find a field-induced magnetically ordered phase reminiscent of a BEC phase, with exceptionally low critical fields of Hc1∼0.4 and Hc2∼1.4 T. Using inelastic neutron scattering in an applied magnetic field we observe a Goldstone mode (gapless to within δE=0.037 meV) that persists throughout the entire field-induced magnetically ordered phase, suggestive of the spontaneous breaking of U(1) symmetry expected for a triplon BEC. However, in contrast to other well-known cases of this phase, the high-field (μ0H≥1.2 T) part of the phase diagram in Yb2Si2O7 is interrupted by an unusual regime signaled by a change in the field dependence of the ultrasound velocity and magnetization, as well as the disappearance of a sharp anomaly in the specific heat. These measurements raise the question of how anisotropy in strongly spin-orbit coupled materials modifies the field induced phases of QDMs.
| Original language | English |
|---|---|
| Article number | 027201 |
| Journal | Physical Review Letters |
| Volume | 123 |
| Issue number | 2 |
| DOIs | |
| State | Published - Jul 9 2019 |
Funding
This research was supported by the National Science Foundation Agreement No. DMR-1611217. J. Q. acknowledges technical support from M. Castonguay and S. Fortier, informative conversations with G. Quirion, C. Bourbonnais, and I. Garate and funding from NSERC. The authors acknowledge the assistance of Aaron Glock and Antony Sikorski in the sample synthesis, as well as Craig Brown for his assistance with the BT1 neutron powder diffraction experiment. A portion of this work used resources at the Spallation Neutron Source and High Flux Isotope Reactor, which are DOE Office of Science User Facilities operated by Oak Ridge National Laboratory. The authors also acknowledges the support of the National Institute of Standards and Technology, U.S. Department of Commerce in providing some of the neutron research facilities used in this work.
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