Dynamics of the velocity fluctuations in sedimenting suspensions of rigid fibres
Alessandro Chiarini, Emanuele Gallorini, Marco Edoardo Rosti
TL;DR
This study uses direct numerical simulations with immersed-boundary coupling to investigate how rigid fibre suspensions settling under gravity generate and organize fluid-phase velocity fluctuations. By varying the Galileo number $Ga$ and the fibre concentration $n\ell_f^3$, the authors show that high $Ga$ and low concentration promote gravity-aligned streamers that enhance small-scale fluid activity and shift energy toward finer scales, while also increasing anisotropy and nonlinear interactions. The work dissects energy budgets across scales, revealing distinct mechanisms sustaining vertical versus in-plane fluctuations and identifying intermittent energy transfer with forward cascades punctuated by backscatter, analyzed through the Kármán–Howarth–Monin–Hill framework. Local structure analyses of the velocity gradient tensor reveal a Ga-dependent transition from axisymmetric compression and 2D strain to axisymmetric extension and HIT-like dynamics, with fibres generally aligning with gravity and heavily clustering in descending streams. Overall, the findings illuminate how $Ga$ and fibre concentration shape the multiscale, anisotropic fluctuations in fibre-laden settling flows, offering a framework to extend to flexible fibres and non-Newtonian fluids.
Abstract
We use direct numerical simulations to investigate fluid-solid interactions in suspensions of rigid fibres settling under gravity in a quiescent fluid. The solid-to-fluid density ratio is $\mathcal{O}(100)$, while the Galileo number ($Ga$) and fibre concentration ($n\ell_f^3$) are varied over the ranges $Ga \in [180, 900]$ and $n\ell_f^3 \in [0.36, 23.15]$; $\ell_f$ denotes the fibre length and $n$ the number density. At high $Ga$ and/or low $n\ell_f^3$, fibres cluster into gravity-aligned streamers with elevated concentrations and enhanced settling velocities, disrupting the flow homogeneity. As $Ga$ increases and/or $n\ell_f^3$ decreases, the fluid-phase kinetic energy rises and the energy spectrum broadens, reflecting enhanced small-scale activity. The flow anisotropy is assessed by decomposing the energy spectrum into components aligned with and transverse to gravity. Vertical fluctuations are primarily driven by fluid-solid interactions, while transverse ones are maintained by pressure-strain effects that promote isotropy. With increasing $Ga$, nonlinear interactions become more prominent, producing a net forward energy cascade toward smaller scales, punctuated by localised backscatter events. Analysis of the local velocity gradient tensor reveals distinct flow topologies: at low $Ga$, the flow is dominated by axisymmetric compression and two-dimensional straining; at high $Ga$, regions of high fibre concentration are governed by two-dimensional strain, while voids are associated with axisymmetric extension. The fluid motion is predominantly extensional rather than rotational.
