论文标题
在过渡到倒液膜的滴
On the transition to dripping of an inverted liquid film
论文作者
论文摘要
研究以零雷诺数的数量研究了在倾斜板下液体薄膜的重力驱动流动的过渡。假设模型层次结构的固定流体体积或固定流速在周期域上进行计算:两个具有线性曲率或完整曲率(分别为LCM和FCM)的润滑模型,以及Stokes流的全方程。特别感兴趣的是随着板倾斜角的增加而崩溃。对于任何固定体积,LCM到达达到余弦轮廓的水平状态。对于足够小的体积,FCM和Stokes溶液达到了弱的年轻宽面平衡曲线,该方法通过渐近分析的概括为LCM的Kalliadasis&Chang(1994)描述了这种方法。对于大容量,FCM和Stokes模型的分叉曲线具有转折点,因此永远无法达到完全倒置的状态。对于固定流量,LCM以临界角度吹动,该角度通过渐近分析进行了很好的预测。 FCM的分叉曲线要么具有转折点,要么达到表面轮廓具有无限斜率奇异性的点,表明多价值的发作。后者通过Stokes模型确认,可以继续获得倾覆的表面曲线。总体而言,薄膜模型要么为滴发作提供了准确的预测,要么在临界倾斜角度提供上限。
The transition to dripping in the gravity-driven flow of a liquid film under an inclined plate is investigated at zero Reynolds number. Computations are carried out on a periodic domain assuming either a fixed fluid volume or a fixed flow rate for a hierarchy of models: two lubrication models with either linearised curvature or full curvature (the LCM and FCM, respectively), and the full equations of Stokes flow. Of particular interest is the breakdown of travelling-wave solutions as the plate inclination angle is increased. For any fixed volume the LCM reaches the horizontal state where it attains a cosine-shaped profile. For sufficiently small volume, the FCM and Stokes solutions attain a weak Young-Laplace equilibrium profile, the approach to which is described by an asymptotic analysis generalising that of Kalliadasis & Chang (1994) for the LCM. For large volumes, the bifurcation curves for the FCM and Stokes model have a turning point so that the fully inverted state is never reached. For fixed flow rate the LCM blows up at a critical angle that is well predicted by asymptotic analysis. The bifurcation curve for the FCM either has a turning point or else reaches a point at which the surface profile has an infinite slope singularity, indicating the onset of multi-valuedness. The latter is confirmed by the Stokes model which can be continued to obtain overturning surface profiles. Overall the thin-film models either provide an accurate prediction for dripping onset or else supply an upper bound on the critical inclination angle.