Mukhopadhyay Sanghasri, Mukhopadhyay Asim
Laboratoire LOCIE, Université Savoie Mont Blanc, Chambéry 73000, France.
Vivekananda Mahavidyalaya, Burdwan 713103, West Bengal, India.
Phys Rev E. 2020 Aug;102(2-1):023117. doi: 10.1103/PhysRevE.102.023117.
Evolution of waves and hydrodynamic instabilities of a thin viscoelastic fluid film flowing down an inclined wavy bottom of moderate steepness have been analyzed analytically and numerically. The classical long-wave expansion method has been used to formulate a nonlinear evolution equation for the development of the free surface. A normal-mode approach has been adopted to discuss the linear stability analysis from the viewpoint of the spatial and temporal study. The method of multiple scales is used to derive a Ginzburg-Landau-type nonlinear equation for studying the weakly nonlinear stability solutions. Two significant wave families, viz., γ_{1} and γ_{2}, are found and discussed in detail along with the traveling wave solution of the evolution system. A time-dependent numerical study is performed with Scikit-FDif. The entire investigation is conducted primarily for a general periodic bottom, and the detailed results of a particular case study of sinusoidal topography are then discussed. The case study reveals that the bottom steepness ζ plays a dual role in the linear regime. Increasing ζ has a stabilizing effect in the uphill region, and the opposite occurs in the downhill region. While the viscoelastic parameter Γ has a destabilizing effect throughout the domain in both the linear and the nonlinear regime. Both supercritical and subcritical solutions are possible through a weakly nonlinear analysis. It is interesting to note that the unconditional zone decreases and the explosive zone increases in the downhill region rather than the uphill region for a fixed Γ and ζ. The same phenomena occur in a particular region if we increase Γ and keep ζ fixed. The traveling wave solution reveals the fact that to get the γ_{1} family of waves we need to increase the Reynolds number a bit more than the value at which the γ_{2} family of waves is found. The spatiotemporal evolution of the nonlinear surface equation indicates that different kinds of finite-amplitude permanent waves exist.
分析了沿中等坡度倾斜波浪形底部流动的薄粘弹性流体薄膜的波动演化和流体动力学不稳定性,采用了解析和数值方法。运用经典的长波展开方法建立了自由表面发展的非线性演化方程。采用正规模式方法从空间和时间研究的角度讨论线性稳定性分析。利用多尺度方法推导了一个用于研究弱非线性稳定性解的金兹堡-朗道型非线性方程。发现并详细讨论了两个重要的波族,即γ₁和γ₂,以及演化系统的行波解。使用Scikit-FDif进行了与时间相关的数值研究。整个研究主要针对一般周期性底部进行,然后讨论了正弦地形特定案例研究的详细结果。案例研究表明,底部坡度ζ在线性区域中起双重作用。增加ζ在上坡区域有稳定作用,而在下坡区域则相反。而粘弹性参数Γ在整个区域的线性和非线性区域都有不稳定作用。通过弱非线性分析,超临界和亚临界解都是可能的。有趣的是,对于固定的Γ和ζ,下坡区域而非上坡区域的无条件区域减小,爆炸区域增大。如果我们增加Γ并保持ζ固定,在特定区域也会出现相同的现象。行波解揭示了这样一个事实,即要得到γ₁波族,我们需要将雷诺数增加到比找到γ₂波族时的值稍大一些。非线性表面方程的时空演化表明存在不同种类的有限振幅永久波。