• Open Access

Quantum Versus Classical Spin Fragmentation in Dipolar Kagome Ice Ho3Mg2Sb3O14

Zhiling Dun, Xiaojian Bai, Joseph A. M. Paddison, Emily Hollingworth, Nicholas P. Butch, Clarina D. Cruz, Matthew B. Stone, Tao Hong, Franz Demmel, Martin Mourigal, and Haidong Zhou
Phys. Rev. X 10, 031069 – Published 29 September 2020

Abstract

A promising route to realize entangled magnetic states combines geometrical frustration with quantum-tunneling effects. Spin-ice materials are canonical examples of frustration, and Ising spins in a transverse magnetic field are the simplest many-body model of quantum tunneling. Here, we show that the tripod-kagome lattice material Ho3Mg2Sb3O14 unites an icelike magnetic degeneracy with quantum-tunneling terms generated by an intrinsic splitting of the Ho3+ ground-state doublet, which is further coupled to a nuclear spin bath. Using neutron scattering and thermodynamic experiments, we observe a symmetry-breaking transition at T*0.32K to a remarkable state with three peculiarities: a concurrent recovery of magnetic entropy associated with the strongly coupled electronic and nuclear degrees of freedom; a fragmentation of the spin into periodic and icelike components; and persistent inelastic magnetic excitations down to T0.12K. These observations deviate from expectations of classical spin fragmentation on a kagome lattice, but can be understood within a model of dipolar kagome ice under a homogeneous transverse magnetic field, which we survey with exact diagonalization on small clusters and mean-field calculations. In Ho3Mg2Sb3O14, hyperfine interactions dramatically alter the single-ion and collective properties, and suppress possible quantum correlations, rendering the fragmentation with predominantly single-ion quantum fluctuations. Our results highlight the crucial role played by hyperfine interactions in frustrated quantum magnets and motivate further investigations of the role of quantum fluctuations on partially ordered magnetic states.

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  • Received 24 December 2019
  • Revised 24 June 2020
  • Accepted 31 July 2020

DOI:https://doi.org/10.1103/PhysRevX.10.031069

Published by the American Physical Society under the terms of the Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI.

Published by the American Physical Society

Physics Subject Headings (PhySH)

Condensed Matter, Materials & Applied Physics

Authors & Affiliations

Zhiling Dun1,2,*,∥, Xiaojian Bai1,∥, Joseph A. M. Paddison1,3,4,†, Emily Hollingworth1, Nicholas P. Butch5, Clarina D. Cruz6, Matthew B. Stone6, Tao Hong6, Franz Demmel7, Martin Mourigal1,‡, and Haidong Zhou2,8,§

  • 1School of Physics, Georgia Institute of Technology, Atlanta, Georgia 30332, USA
  • 2Department of Physics and Astronomy, University of Tennessee, Knoxville, Tennessee 37996, USA
  • 3Churchill College, University of Cambridge, Storey’s Way, Cambridge CB3 0DS, United Kingdom
  • 4Materials Science and Technology Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
  • 5NIST Center for Neutron Research, Gaithersburg, Maryland 20899, USA
  • 6Neutron Scattering Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37831, USA
  • 7ISIS Facility, Rutherford Appleton Laboratory, Didcot OX11 0QX, United Kingdom
  • 8National High Magnetic Field Laboratory, Florida State University, Tallahassee, Florida 32310, USA

  • *zdun3@gatech.edu
  • paddisonja@ornl.gov
  • mourigal@gatech.edu
  • §hzhou10@utk.edu
  • Z. D. and X. B. contributed equally to this work.

Popular Summary

Quantum spin ice is a highly entangled state that researchers have long tried to achieve in the lab because of its theoretical simplicity and its close relation to real pyrochlore minerals. But it is very difficult to endow the underlying spins with robust quantum dynamics on the pyrochlore lattice without introducing additional complications and departing from the necessarily simplified theoretical models. Our work exploits a new concept for realizing a 2D quantum spin ice by using a low-symmetry crystal structure to increase quantum fluctuations, an approach that will help others find and design new quantum materials.

Specifically, we study the material Ho3Mg2Sb3O14, a “tripod kagome magnet” derived from the pyrochlore lattice. This system offers the geometrical frustration of spin ice and a material-based approach to introducing a homogenous transverse magnetic field that make it ideal for this kind of work. Using neutron-scattering experiments, we find a spin-fragmented state at low temperature with persistent quantum dynamics, which is strongly affected by hyperfine interactions. This discovery highlights how nuclear spins contribute to the dynamics of frustrated magnets and exemplifies how low-symmetry crystal structures can be used to increase quantum fluctuations for spin-ice-like materials in general.

With these findings, we hope that researchers will now consider it a practical option to introduce quantum fluctuations in frustrated magnets and pay close attention to the role of nuclear spins in their quest to create quantum spin ices.

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Vol. 10, Iss. 3 — July - September 2020

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