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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.

Spontaneous Ratchet Currents and Transition Dynamics in Active Wetting

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 for barrier-induced transitions, with , tending to as . The study shows that the partially-wet state supports a steady ratchet current that scales as 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.

Paper Structure

This paper contains 4 sections, 24 equations, 4 figures.

Figures (4)

  • Figure 1: (a.1) Illustration of the system geometry. (a.2) Surface phase diagram; individual points are labelled according to their extrapolated steady-state. (b.1-2) Example full- and partial-wetting states; orientation-dependent density $f(x, \theta, t)$ is shown in colour; arrows show current (arbitrary scale); integrated spatial density $\rho(x, t)$ is shown with overlaid line. (c) Critical wetting phenomena. (c.1) Divergence of the thin film width. (c.2) Pitchfork bifurcation in the asymmetry, scanning $\mathcal{A}$ as a function of $\epsilon$ up (orange) and down (blue). (c.3) Linear stability of a fully-wet initial condition with weak noise; measured at early times, when asymmetry growth is approximately linear. See companion_paper_placeholder for further details of numerics.
  • Figure 2: Illustration of steady-state current in the partially-wet state. (a) Steady-state current as a function of system size, tending to $\sim1/\ell_s$. (b) Steady-state current vanishes continuously as $\epsilon \to \epsilon^*$ (same parameters as Figure \ref{['fig:wetting_states']}(c.2)).
  • Figure 3: (a.1) Full-to-partial transition pathway at $\text{Pe}=15$. (a.2) $\mathcal{A}(t)$ for this process. (b.1, b.2) Pathway and asymmetry for partial-to-full transition at $\text{Pe}=8$.
  • Figure 4: (a) Density profile over time for a full-to-partial transition in the minimal model ($\alpha = \kappa = 1, \eta = 2$). (b) Asymmetry over time. Comparing with Fig \ref{['fig:dynamical_pathways']}(a) one sees that the minimal model captures the three-stage transition found in the full dynamics.