School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138.
Physics of Environmental Systems, Department of Environmental System Sciences, ETH Zürich, 8092 Zürich, Switzerland.
Proc Natl Acad Sci U S A. 2018 Sep 18;115(38):9479-9484. doi: 10.1073/pnas.1803644115. Epub 2018 Sep 5.
The formation of droplets is ubiquitous in many natural and industrial processes and has reached an unprecedented level of control with the emergence of milli- and microfluidics. Although important insight into the mechanisms of droplet formation has been gained over the past decades, a sound understanding of the physics underlying this phenomenon and the effect of the fluid's flow and wetting properties on the droplet size and production rate is still missing, especially for the widely applied method of step emulsification. In this work, we elucidate the physical controls of microdroplet formation in step emulsification by using the wetting of fluidic channels as a tunable parameter to explore a broad set of emulsification conditions. With the help of high-speed measurements, we unequivocally show that the final droplet pinch-off is triggered by a Rayleigh-Plateau-type instability. The droplet size, however, is not determined by the Rayleigh-Plateau breakup, but by the initial wetting regime, where the fluid's contact angle plays a crucial role. We develop a physical theory for the wetting process, which closely describes our experimental measurements without invoking any free fit parameter. Our theory predicts the initiation of the Rayleigh-Plateau breakup and the transition from dripping to jetting as a function of the fluid's contact angle. Additionally, the theory solves the conundrum why there is a minimal contact angle of = 2π/3 = 120° for which droplets can form.
液滴的形成在许多自然和工业过程中无处不在,随着毫微和微流控技术的出现,液滴的形成已经达到了前所未有的控制水平。尽管在过去的几十年里,人们已经对液滴形成的机制有了重要的了解,但对于这种现象背后的物理原理以及流体流动和润湿性对液滴大小和生成速率的影响,人们仍然缺乏深入的理解,特别是对于广泛应用的阶跃乳化法。在这项工作中,我们通过将流体通道的润湿作为一个可调参数,阐明了阶跃乳化中微液滴形成的物理控制。借助高速测量,我们明确地表明,最终的液滴断裂是由瑞利-普兰特尔型不稳定性触发的。然而,液滴大小不是由瑞利-普兰特尔断裂决定的,而是由初始润湿状态决定的,其中流体的接触角起着关键作用。我们提出了一个关于润湿过程的物理理论,该理论无需引入任何自由拟合参数,就能很好地描述我们的实验测量。我们的理论预测了瑞利-普兰特尔断裂的开始以及从滴状到射流的转变,这是作为流体接触角的函数。此外,该理论还解决了为什么存在最小接触角 = 2π/3 = 120°的难题,在这个接触角下液滴才能形成。