Settling dynamics of an oloid: experiments and simulations
Mees M. Flapper, Giulia Piumini, Roberto Verzicco, Sander G. Huisman, Detlef Lohse
TL;DR
This study addresses how the oloid’s unique curved geometry governs the settling of anisotropic particles in quiescent fluids. It employs a combined experimental (two sizes, ranged $Ga$, density contrasts via water–glycerol) and numerical (immersed boundary with Newton–Euler dynamics) approach to identify two distinct falling modes: a stable, orientation-preserving regime with rotation about the vertical axis and a tilted orientation, and a tumbling regime with random orientation. Orientation and rotation statistics reveal a translation–rotation coupling in the stable regime and a transition toward randomness as $Ga$ increases, with the stable mode obeying Stokes-like drag and the tumbling mode dominated by turbulent drag. The findings advance understanding of shape–drag–rotation interactions for anisotropic particles and provide benchmarks for validating fluid–structure interaction models in applications ranging from sedimentation to robotic design.
Abstract
This study presents a combined experimental and computational investigation of an oloid shaped particle settling in a quiescent fluid. The oloid, a unique convex shape with anisotropic geometry, provides a distinctive model for exploring how a particle's shape and orientation affect its settling dynamics. The settling oloids are tracked experimentally for Galileo numbers $48 \leq \text{Ga} \leq 5.4 \cdot 10^3$, using two particle sizes ($D_{\text{eq}}$ = 21.6 mm, and $D_{\text{eq}}$ = 10.8 mm). The density ratio between the particle and fluid $Γ$ = $\frac{ρ_p}{ρ_f}$ ranges from $1.11 \leq Γ\leq 1.30$ in the experiments. Computationally, the Galileo numbers $10 \leq \text{Ga} \leq 100$ are simulated, with $Γ= 2$. The experimental findings and numerical results are in good agreement, and give a consistent idea of the oloid settling dynamics. Our results indicate two distinct falling modes for the oloid, separated by Galileo number. The stable mode is characterised by a preferential orientation, with a rotation around the vertical axis, whereas the tumbling mode has randomly distributed orientation and rotation statistics. We characterise the falling velocity, orientation, and rotation dynamics of the oloids over a range of Galileo numbers. Additionally, the influence of the initial orientation is revealed to determine the rotation dynamics at low Galileo numbers.
