Quadrupole-conserving dynamics in the non-commutative plane
Isabella Zane, Andrew Lucas
TL;DR
This work introduces a new dynamical universality class arising from area-preserving dynamics on the non-commutative plane, governed by the symmetry group $G=\mathrm{SL}(2,\mathbb{R})\rtimes \mathbb{R}^2$ that enforces dipole and quadrupole conservation. It develops both non-dissipative and dissipative effective field theories, rooted in polygon (notably triangle) area invariants, and analyzes lattice realizations to reveal a consistent $\omega\propto k^3$ phonon dispersion and the breakdown of linear hydrodynamics due to relevant nonlinearities. The authors demonstrate, via a Trotter-split numerical scheme that exactly preserves conserved charges, that the long-wavelength dynamics flow to a universality with dynamical exponent $z\approx 3$, independent of initial energy density over accessible times. While experimental realization remains challenging, the study outlines potential quantum Hall or vortex-fluid platforms and toy classical implementations that could realize this quadrupole-conserving fracton-like dynamics, offering a new lens on fracton hydrodynamics in two dimensions.
Abstract
Inspired by ``fracton hydrodynamic" universality classes of dynamics with unusual conservation laws, we present a new dynamical universality class that arises out of local area-preserving dynamics in the non-commutative plane. On this symplectic manifold, the area-preserving spatial symmetry group $\mathrm{SL}(2,\mathbb{R})\rtimes \mathbb{R}^2$ is a symmetry group compatible with non-trivial many-body dynamics. The conservation laws associated to this symmetry group correspond to the dipole and quadrupole moments of the particles. We study the unusual dynamics of a crystal lattice subject to such symmetries, and argue that the hydrodynamic description of lattice dynamics breaks down due to relevant nonlinearities. Numerical simulations of classical Hamiltonian dynamical systems with this symmetry are largely consistent with a tree-level effective field theory estimate for the endpoint of this instability.
