We study the hydrodynamic interactions between colloids suspended in a compressible fluid inside a rigid channel. Using lattice–Boltzmann simulations and a simplified hydrodynamic theory, we find that the diffusive dynamics of density...
moreWe study the hydrodynamic interactions between colloids suspended in a compressible fluid inside a rigid channel. Using lattice–Boltzmann simulations and a simplified hydrodynamic theory, we find that the diffusive dynamics of density perturbations (sound) in the confined fluid give rise to particle correlations of exceptionally long spatial range and algebraic temporal decay. We examine the effect of these sound-mediated correlations on two-particle dynamics and on the collective dynamics of a quasi-one-dimensional suspension. 1. Introduction Particles embedded in an unbounded fluid are dynamically correlated by hydrodynamic interactions that decay like 1/r (where r denotes the separation between particles) [1]. This result is understood in terms of the fundamental solution to the steady-state Stokes equation, η∇ 2 u = ∇p − bδ(r), supplemented by the fluid-incompressibility condition ∇ · u = 0. Here u is the flow velocity field, p the pressure field, b a point force, and η the shear viscosity. It follows from the first equation that the vorticity, ∇×u, satisfies the Laplace equation, leading in the case of an unbounded fluid to the 1/r slow decay of the velocity field. When particles are confined to a quasi-one-dimensional (q1D) channel, however, these long-range dynamic correlations are cut off [2], the screening being attributed to dissipation at the fluid-solid interface, i.e., to the loss of fluid momentum at the channel boundaries. The resulting screening length is comparable to the channel width. The dissipative effect of the boundaries can be incorporated through an additional friction term in an " effective fluid " model [3, 4], η∇ 2 u = ρ 0 ξu + ∇p − bδ(r). In the extra term ρ 0 is the fluid mass density and ξ an effective friction coefficient. The parameter ξ has units of inverse time and characterizes the rate of momentum loss to the boundaries. It can be estimated, therefore, as the inverse of the time it takes fluid momentum to diffuse to the channel boundary, ξ ∼ ν/h 2 , ν = η/ρ 0 being the kinematic shear viscosity and h the channel width. This simplified, phenomenological approach has been shown by simulations [5, 6, 7, 8] and analytical calculations [9] to correctly reproduce the qualitative behavior of confined fluids. The modified Stokes equation leads to a Helmholtz equation for the vorticity, whose regular solutions are exponentially screened functions. Yet, the friction that suppresses the vorticity (transverse fluid stress) does not similarly suppress the pressure field (longitudinal fluid stress) emanating from a locally applied force. Consequently, the application of a localized force generates a long-range pressure distribution, which may give rise to long-range flows and forces on embedded particles. For example, in a q2D suspension confined between two plates, the pressure distribution creates