表面润湿性不均匀的毛细通道中界面运动的控制

Mehmet Alptug BOYLU, Umut CEYHAN
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引用次数: 0

摘要

由于外部流动驱动机制的减少或消除,自驱动流在微流控装置中的应用吸引了许多研究人员的关注。提供这种运动的机制之一是在毛细管运动的情况下,在界面上产生压力差。毛细作用,即由于其曲率导致的界面上的压力差,驱动了运动。这种压力取决于与毛细管壁的相互作用,如果改变毛细管壁的表面能,这种压力是可控的。在这项研究中,我们寻找表面能对毛细管驱动流动中界面运动的影响。为此,我们建立了流体颗粒在毛细管通道中的运动模型,并使用二元晶格玻尔兹曼方法对两相流的控制方程进行了积分。首先,我们验证了我们的求解器对于典型的静态和动态问题。然后,我们讨论两个主要贡献;我们展示了如何使界面速度偏离具有均匀壁能的通道中运动的界面速度,并讨论了这种界面停滞的条件(如通道中的被动阀)。调整通道壁的润湿性,我们提供了一个简单的停止界面的条件:界面与底部和顶部通道壁的平衡接触角之和需要满足$\theta_{eq}^{top}+\theta_{eq}^{bot} \geq \pi$。不同润湿区域的结构和润湿特性共同起着重要的作用
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Controlling the Motion of Interfaces in Capillary Channels with Non-uniform Surface Wettability
The use of self-driven flows in microfluidic devices attracts many researchers as the external flow-driving mechanism is diminished or eliminated. One of the mechanisms providing such motions is generating a pressure difference across interfaces as in the case of the motion in capillary tubes. The capillarity, namely, the pressure difference across the interface due to its curvature drives the motion. This pressure depends on the interaction with the capillary walls and is controlled if one varies the surface energy of the walls. In this study, we search for the effects of surface energy on the motion of interfaces in capillary-driven flow. To this end, we model the motion of fluid particles in a capillary channel and integrate the governing equations using the binary lattice Boltzmann method for the two-phase flow. We, first, validate our solver for canonical static and dynamic problems. We, then, discuss two main contributions; we show how to deviate the interface speed from the ones moving in channels with uniform wall energies and discuss the conditions under which such an interface stagnates (like a passive valve in a channel). Tuning the wettability of the channel walls, we provide a simple condition for stopping the interface: the summation of the equilibrium contact angles interface make with the channel walls at the bottom and top wall need to satisfy $\theta_{eq}^{top}+\theta_{eq}^{bot} \geq \pi$. Configurations and wetting properties of different wettability regions play major roles together
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