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Ratchet mechanism of drops climbing a vibrated oblique plate

Published online by Cambridge University Press:  01 December 2017

Hang Ding*
Affiliation:
Department of Modern Mechanics, University of Science and Technology of China, Hefei 230027, China
Xi Zhu
Affiliation:
Department of Modern Mechanics, University of Science and Technology of China, Hefei 230027, China
Peng Gao
Affiliation:
Department of Modern Mechanics, University of Science and Technology of China, Hefei 230027, China
Xi-Yun Lu
Affiliation:
Department of Modern Mechanics, University of Science and Technology of China, Hefei 230027, China
*
†Email address for correspondence: hding@ustc.edu.cn

Abstract

In this paper, we investigate the ratchet mechanism of drops climbing a vibrated oblique plate based on three-dimensional direct numerical simulations, which for the first time reproduce the existing experiment (Brunet et al., Phys. Rev. Lett., vol. 99, 2007, 144501). With the help of numerical simulations, we identify an interesting and important wetting behaviour of the climbing drop; that is, the breaking of symmetry due to the inclination of the plate with respect to the acceleration leads to a hysteresis of the wetted area in one period of harmonic vibration. In particular, the average wetted area in the downhill stage is larger than that in the uphill stage, which is found to be responsible for the uphill net motion of the drop. A new hydrodynamic model is proposed to interpret the ratchet mechanism, taking account of the effects of the acceleration and contact angle hysteresis. The predictions of the theoretical analysis are in good agreement with the numerical results.

Information

Type
JFM Rapids
Copyright
© 2017 Cambridge University Press 
Figure 0

Figure 1.Sketch of a moving drop on an inclined plate that vibrates vertically at an acceleration of $a=\unicode[STIX]{x1D706}_{a}a_{0}\sin \unicode[STIX]{x1D719}$.

Figure 1

Figure 2.Snapshots of a climbing drop at different phases with $Re=30.9$, $We=9.17$, $St=0.185$, $Fr=17.8$, $\unicode[STIX]{x1D706}_{a}=1.03$, $\unicode[STIX]{x1D703}_{A}=77^{\circ }$, $\unicode[STIX]{x1D703}_{R}=44^{\circ }$ and $\unicode[STIX]{x1D6FC}=45^{\circ }$. (a–d) Comparison with the experimental data obtained by Brunet et al. (2007) under the same flow conditions. Side views of the drop from the numerical results (white curves) are superimposed on the experimental snapshots. (e–h) Top view of the drop shape in the numerical simulations at the same phases as in (a–d).

Figure 2

Figure 3.Convergence study for the shape of the CL at $\unicode[STIX]{x1D719}=7/10\unicode[STIX]{x03C0}$. The flow parameters are the same as in figure 2. The numerical results are obtained on meshes of different resolutions: $\unicode[STIX]{x0394}x=1/40$ (dashed), $1/60$ (solid) and $1/70$ (dash-dotted).

Figure 3

Figure 4.The variation of the flow quantities in one period of acceleration. It should be noted that this is the same case as in figure 2. (a) The variation of the CL speed $u_{CL}$ at the upper end (dash-dotted line) and lower end (solid line) of the CL. (b) The variation of the volume-averaged drop velocity $u_{c}$ (solid line), which is close to a harmonic function (dotted line). The bullets indicate the corresponding phases shown in figure 2. (c) The non-harmonic variation of the wetted area $S_{CL}$. The dashed line represents an image of the variation of the wetted area in the uphill stage. The region in grey corresponds to the difference in the wetted area between the uphill and downhill stages in one period, i.e. $\unicode[STIX]{x03C0}\cdot \unicode[STIX]{x0394}S$.

Figure 4

Figure 5.Numerical results in the absence of gravity and contact angle hysteresis ($\unicode[STIX]{x1D703}_{A}=\unicode[STIX]{x1D703}_{R}=60^{\circ }$) at $We=6.6$ and $Re=23.6$. (a) The variation of $\cos \unicode[STIX]{x0394}\unicode[STIX]{x1D719}$ as a function of $St$. The solid line is a linear fitting of the data. (b) The variation of $\unicode[STIX]{x0394}S/S_{m}$ as a function of $\unicode[STIX]{x1D706}_{a}$. (c) Comparison of the net drop velocity between numerical results and the predictions of (3.6); the dashed lines represent linear fittings. It should be noted that the same cases are included in (b) and (c), with $St=0.115$ (▪), 0.148 (▵), 0.184 (●), 0.231 (♢) and 0.294 (▸).

Figure 5

Figure 6.Numerical results in the absence of gravity at $We=6.6$, $Re=23.6$ and $\unicode[STIX]{x1D703}_{A}=60^{\circ }$. (a) The contact angle distribution at $\unicode[STIX]{x1D719}=\unicode[STIX]{x03C0}$, with $St=0.148$, $\unicode[STIX]{x1D706}_{a}=1.75$ and $\unicode[STIX]{x1D703}_{R}=30^{\circ }$. (b,c) The same cases at $St=0.115$; the results are denoted by the same symbols. The variation of $\unicode[STIX]{x0394}S/S_{m}$ and the net drop velocity $Ca$ at different values of $\unicode[STIX]{x0394}\unicode[STIX]{x1D703}$ are shown in (b) and (c) respectively. The dashed lines in (c) represent data fittings (quadratic for $\unicode[STIX]{x1D706}_{a}\leqslant 1$ and linear for $\unicode[STIX]{x1D706}_{a}\geqslant 1.25$).