Physics of Drop Coalescence on a Surface with Graded Wettability

Manjinder Singh
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Abstract

Drops on a surface that has graded wettability move when the wettability gradient is greater than hysteresis. We experimentally demonstrate that coalescence of drops initiate the motion of resultant drop on a surface that has hysteresis greater than wettability gradient. Importantly, our experiments show that in addition to shift of center of mass towards high wetting region, drop coalescence on a surface having graded wettability also results in motion of merged drop. We also explain the mechanism by which drop coalescence on a surface having graded wettability results in motion of otherwise stationary drops. Based on the mechanism, we analytically show that on a surface that has wettability gradient larger than hysteresis coalescence leads to reduction in drop size at which drop starts to move. Our analytical results show that reduction of drop departure radius due to coalescence depends on the local wetting conditions of the surface with wettability gradient.
具有渐变润湿性的表面上液滴聚结的物理学
当润湿性梯度大于滞后性时,润湿性梯度上的液滴移动。我们通过实验证明,液滴的聚并引起了液滴在滞回大于润湿性梯度的表面上的运动。重要的是,我们的实验表明,除了质心向高润湿区移动之外,在具有渐变润湿性的表面上的液滴聚结也导致了合并液滴的运动。我们还解释了液滴在具有渐变润湿性的表面上聚结导致其他静止液滴运动的机制。基于这一机理,我们分析表明,在润湿性梯度大于滞后的表面上,聚结导致液滴尺寸减小,液滴开始移动。我们的分析结果表明,由于聚结导致的液滴离开半径的减小取决于具有润湿性梯度的表面局部润湿条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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