Spin-orbital Kitaev model: From kagome spin ice to classical fractons

We study an exactly solvable spin-orbital model that can be regarded as a classical analog of the celebrated Kitaev honeycomb model and describes interactions between Rydberg atoms on the ruby lattice. We leverage its local and nonlocal symmetries to determine the exact partition function and the static structure factor. A mapping between $S=3/2$ models on the honeycomb lattice and kagome spin Hamiltonians allows us to interpret the thermodynamic properties in terms of a classical kagome spin ice. Partially lifting the symmetries associated with line operators, we obtain a model characterized by immobile excitations, called classical fractons, and a ground-state degeneracy that increases exponentially with the length of the system. We formulate a continuum theory that reveals the underlying gauge structure and conserved charges. Extensions of our theory to other lattices and higher-spin systems are suggested.

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Publication Details

Journal
Physical review. B./Physical review. B
Published
2025-05-07
DOI
https://doi.org/10.1103/physrevb.111.195112
Citations
3
Primary Topic
Advanced Condensed Matter Physics
Type
article
Field-Weighted Citation Impact
3.77

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article

Spin-orbital Kitaev model: From kagome spin ice to classical fractons

Rodrigo G. Pereira, Fabrizio Oliviero, Weslei Fontana, W. M. H. Natori
3 citations
Physical review. B./Physical review. B
Advanced Condensed Matter Physics
3.77
article

Spin-orbital Kitaev model: From kagome spin ice to classical fractons

Rodrigo G. Pereira, Fabrizio Oliviero, Weslei Fontana, W. M. H. Natori
article en
3 citations

Abstract

We study an exactly solvable spin-orbital model that can be regarded as a classical analog of the celebrated Kitaev honeycomb model and describes interactions between Rydberg atoms on the ruby lattice. We leverage its local and nonlocal symmetries to determine the exact partition function and the static structure factor. A mapping between $S=3/2$ models on the honeycomb lattice and kagome spin Hamiltonians allows us to interpret the thermodynamic properties in terms of a classical kagome spin ice. Partially lifting the symmetries associated with line operators, we obtain a model characterized by immobile excitations, called classical fractons, and a ground-state degeneracy that increases exponentially with the length of the system. We formulate a continuum theory that reveals the underlying gauge structure and conserved charges. Extensions of our theory to other lattices and higher-spin systems are suggested.

Physical review. B./Physical review. BVol. 111(19)
Universidade Estadual de Campinas (UNICAMP) (BR), National Tsing Hua University (TW), Universidade Federal do Rio Grande do Norte (BR), Institut Langevin (FR), National Center for Theoretical Sciences (TW)
National Center for Theoretical Sciences, Ministry of Science and Technology, Taiwan
Climate action
Openalex Percentile: Top 7%
Advanced Condensed Matter Physics
3.77
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