Symmetry re-breaking in an effective theory of quantum coarsening
Federico Balducci, Anushya Chandran, Roderich Moessner
TL;DR
This work addresses out-of-equilibrium quantum coarsening in 2D and explains two key experimental observations—the speeding up of coarsening near the phase boundary and persistent order-parameter oscillations after quenches within the ordered phase—using a minimal classical-spin framework derived from the transverse-field Ising model. By combining energy-conserving classical dynamics with mean-field and Gaussian-fluctuation analyses, the authors show that the observed phenomena arise from purely semiclassical dynamics: a dual role of the kinetic term enhances coarsening deep in the ordered phase while the vanishing domain-wall tension near criticality slows it, and mean-field oscillations are captured by a two-dimensional Lipkin-Meshkov-Glick dynamics with a dynamical separatrix at $g_{\mathrm{dyn}}=2$. The central new concept, symmetry re-breaking, emerges when spatial fluctuations drive local MF trajectories across the MF separatrix, creating domains that coarsen within the ordered phase and leave the final magnetization sign determined by the oscillation count. These results suggest that semiclassical approaches can disentangle genuine quantum effects from dynamical features in quantum coarsening and point to broader applicability of symmetry re-breaking in symmetry-broken Hamiltonian systems across experimental platforms.
Abstract
We present a simple theory accounting for two central observations in a recent experiment on quantum coarsening and collective dynamics on a programmable quantum simulator [T. Manovitz et al., Nature \textbf{638}, 86 (2025)]: an apparent speeding up of the coarsening process as the phase transition is approached; and persistent oscillations of the order parameter after quenches within the ordered phase. Our theory, based on the Hamiltonian structure of the equations of motion in the classical limit of the quantum model, finds a speeding up already deep within the ordered phase, with subsequent slowing down as the domain wall tension vanishes upon approaching the critical line. Further, the oscillations are captured within a mean-field treatment of the order parameter field. For quenches within the ordered phase, small spatially-varying fluctuations in the initial mean-field lead to a remarkable long-time effect, wherein the system dynamically destroys its long-range order and has to coarsen to re-establish it. We term this phenomenon \emph{symmetry re-breaking}, as the resulting late-time magnetization can have a sign opposite to the initial magnetization.
