Backflow-Induced Inertial Arrest of Velocity Fluctuations in Sedimenting Suspensions

Abstract

A self-contained hydrodynamic theory is proposed to reconcile the discrepancy between divergent Stokesian velocity fluctuations and finite experimental measurements in sedimenting suspensions. We show that the compensating backflow induces non-negligible inertia, giving rise to an emergent screening length $ξ\sim aϕ^{-1/3}Re_p^{-1/3}$ far exceeding the mean interparticle spacing $aϕ^{-1/3}$ even at vanishingly small particle Reynolds numbers. This backflow inertial screening, together with finite-time viscous diffusion, arrests the indefinite spatiotemporal growth of large-scale velocity fluctuations. The resulting velocity fluctuations scale as $δu \sim ϕ^{1/3}V_sRe_p^{-1/6}$, together with the viscous correlation time $τ_c=ξ^2/ν$, reproducing the well-known hydrodynamic self-diffusivity scaling $D_H\sim V_s a$. The theory predicts the prefactors of these scaling laws without adjustable parameters, in good quantitative agreement with experimental measurements. It also successfully captures the experimentally observed crossover from the finite-correlation regime to the finite-system regime as the screening length becomes comparable to the system size.