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Elastohydrodynamics of a sliding, spinning and sedimenting cylinder near a soft wall

Published online by Cambridge University Press:  14 August 2015

Thomas Salez
Affiliation:
School of Engineering and Applied Sciences and Department of Physics, Harvard University, Cambridge, MA 02138, USAPCT Lab, UMR CNRS 7083 Gulliver, ESPCI ParisTech, PSL Research University, 75005 Paris, France
L. Mahadevan*
Affiliation:
School of Engineering and Applied Sciences and Department of Physics, Harvard University, Cambridge, MA 02138, USA
*
†Email address for correspondence: lm@seas.harvard.edu

Abstract

We consider the motion of a fluid-immersed negatively buoyant particle in the vicinity of a thin compressible elastic wall, a situation that arises in a variety of technological and natural settings. We use scaling arguments to establish different regimes of sliding, and complement these estimates using thin-film lubrication dynamics to determine an asymptotic theory for the sedimentation, sliding and spinning motions of a cylinder. The resulting theory takes the form of three coupled nonlinear singular-differential equations. Numerical integration of the resulting equations confirms our scaling relations and further yields a range of unexpected behaviours. Despite the low-Reynolds-number feature of the flow, we demonstrate that the particle can spontaneously oscillate when sliding, can generate lift via a Magnus-like effect, can undergo a spin-induced reversal effect and also shows an unusual sedimentation singularity. Our description also allows us to address a sedimentation–sliding transition that can lead to the particle coasting over very long distances, similar to certain geophysical phenomena. Finally, we show that a small modification of our theory allows us to generalize the results to account for additional effects such as wall poroelasticity.

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© 2015 Cambridge University Press 
Figure 0

Figure 1.Schematic of the system. A negatively buoyant cylinder (green) falls down under the influence of gravity $\boldsymbol{g}$, inside a viscous fluid (blue), in the vicinity of a thin soft wall (brown). The ensemble lies atop a tilted infinitely rigid support (grey).

Figure 1

Figure 2.Oscillations: when a cylinder is released close to an inclined wall with a non-zero tangential velocity, it spontaneously oscillates about the stable sliding height; however, with time, these oscillations eventually decay. These results follow from the numerical solution of (3.7), for ${\it\alpha}={\rm\pi}/4$, ${\it\xi}=0.1$, ${\it\kappa}=0.1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$, $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)=\dot{{\it\Theta}}(0)=0$ and ${\dot{X}}_{\mathit{G}}(0)=10$.

Figure 2

Figure 3.Magnus-like effect: when the cylinder is released close to the horizontal elastic wall with a non-zero angular velocity, it lifts off. These results follow from the numerical solution of (3.7), for ${\it\alpha}=0$, ${\it\xi}=10$, ${\it\kappa}=0.1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$, $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)=0$ and ${\dot{X}}_{\mathit{G}}(0)=\dot{{\it\Theta}}(0)=10$. If we replace the last condition by $\dot{{\it\Theta}}(0)=0$, then ${\it\Delta}$ diminishes.

Figure 3

Figure 4.Enhanced sedimentation: when the cylinder is allowed to fall freely vertically towards the horizontal elastic wall, it sediments faster than if the wall is rigid. These results follow from the numerical solutions of (3.7), for ${\it\alpha}=0$, ${\it\xi}=1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$ and $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)={\dot{X}}_{\mathit{G}}(0)=\dot{{\it\Theta}}(0)=0$. The dashed line corresponds to the case of a rigid wall, with ${\it\kappa}=0$, showing that ${\it\Delta}$ decreases gradually, while the solid line corresponds to sedimentation towards a soft wall, with ${\it\kappa}=0.1$, where the cylinder abruptly crashes downwards after sedimenting at a rate faster than towards a rigid wall. Panel (b) shows that the horizontal position of the cylinder does not vary at all during sedimentation (the simulation is extended to $T=2$ corresponding to the case of sedimentation towards a rigid wall).

Figure 4

Figure 5.Sedimentation–sliding transition, observed when the cylinder is released close to the inclined elastic wall with the threshold tangential velocity given by (4.5). The results follow from the numerical solution of (3.7), for ${\it\alpha}={\rm\pi}/4$, ${\it\xi}=1$, ${\it\kappa}=0.1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$, $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)=\dot{{\it\Theta}}(0)=0$, ${\dot{X}}_{\mathit{G}}(0)=2.1$ (red dots) and ${\dot{X}}_{\mathit{G}}(0)=2.5$ (green lines). For these parameters, $U_{\mathit{c}}\approx 2.30$ (blue dash-dotted line), as obtained from (4.5).

Figure 5

Figure 6.Spin-induced reversal: when the cylinder is released close to the horizontal elastic wall with non-zero tangential and rotational velocities, it can return backwards. These results follow from the numerical solution of (3.7), for ${\it\alpha}=0$, ${\it\xi}=10$, ${\it\kappa}=0.1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$, $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)=0$, ${\dot{X}}_{\mathit{G}}(0)=1$ and $\dot{{\it\Theta}}(0)=10$.

Figure 6

Figure 7.Convergence to the long-term sliding steady state, observed when the cylinder is released close to the inclined elastic wall with an initial tangential velocity greater than the threshold velocity given by (4.5). The results follow from the numerical solution of (3.7), for ${\it\alpha}={\rm\pi}/4$, ${\it\xi}=1$, ${\it\kappa}=0.1$, ${\it\epsilon}=0.1$, ${\it\Delta}(0)=1$, $X_{\mathit{G}}(0)=\dot{{\it\Delta}}(0)=\dot{{\it\Theta}}(0)=0$ and ${\dot{X}}_{\mathit{G}}(0)=2.5$ (green lines). For those parameters, the terminal height and velocity of the sliding steady state are given by ${\it\Delta}_{\infty }\approx 0.524$ and $U_{\infty }\approx 1.72$ (orange dashed lines), as obtained from (4.6) and (4.7) respectively.