Spontaneous Ratchet Currents and Transition Dynamics in Active Wetting
Noah Grodzinski, Robert L. Jack, Michael E. Cates
TL;DR
This work analyzes active wetting of self-propelled particles on repulsive barriers using an exact noiseless hydrodynamic limit of an active lattice gas in a slit-like geometry, showing robust fully- and partially-wet states and a critical wetting transition. It reveals a spontaneous symmetry-breaking ratchet current in the partially-wet state, driven by activity rather than geometric asymmetry, which alters steady states and introduces a faster, non-equilibrium dynamical pathway between wetting states. To understand this mechanism, the authors develop a minimal model—a scalar field with a double-well free energy and a localized pump—that reproduces the three-stage full-to-partial transition and yields a finite instability threshold $\eta^*$ for barrier-induced transitions, with $\eta^* = \dfrac{\sqrt{2 \alpha \kappa}}{\coth\left(L \sqrt{\frac{\alpha}{8 \kappa}}\right) - \dfrac{1}{L}\sqrt{\frac{8 \kappa}{\alpha}}}$, tending to $\sqrt{2 \alpha \kappa}$ as $L \to \infty$. The study shows that the partially-wet state supports a steady ratchet current $J^{(\rho)}_{ss}$ that scales as $J^{(\rho)}_{ss} \sim \ell_s^{-1}$ for large system size, and that bulk densities depart from their binodal values due to this nonequilibrium drive, highlighting intrinsic nonequilibrium effects in active wetting. Overall, the work connects equilibrium-like surface phase transitions with genuine nonequilibrium phenomena, suggesting experimental routes using, e.g., light-activated colloids in quasi-1D channels to test active wetting predictions.
Abstract
Self-propelled particles accumulate on repulsive barriers in so-called active wetting, but the relationship between this process and equilibrium wetting remains unclear. Using an exact (noiseless) hydrodynamic framework for an active lattice gas, we show, using a slit geometry with periodic boundary conditions, that active matter exhibits both fully- and partially-wet states, with a critical wetting transition between them. Furthermore, we demonstrate the existence of a spontaneous-symmetry-breaking ratchet current in the partially wet state, leading to departure of the bulk densities from their binodal values and the emergence of a novel dynamical pathway for the full-to-partial wetting transition. We elucidate this modified dynamical pathway using a minimal model. The results, while establishing a direct connection between active and equilibrium wetting, also identify the nonequilibrium consequences of activity.
