Surface and internal gravity waves on a viscous liquid layer: Initial-value problems

Ramana Patibandla

doi:10.1016/j.ijmultiphaseflow.2023.104592

2023-12-01

DOI：10.1016/j.ijmultiphaseflow.2023.104592

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摘要

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We study a class of initial value problems (IVPs) involving perturbations on a density stratified, quiescent, viscous liquid layer with a free-surface. The geometry is a two-dimensional, rectangular configuration taking into account surface-tension and gravity. Linearised predictions are obtained by solving the IVP analytically for free-surface and vortical initial perturbations. The viscous spectrum comprises a discrete spectrum of propagating surface and internal modes and damped vorticity modes. Continuous spectra may also exist depending on whether the domain is bounded or unbounded. It is shown that independent of stratification, the vorticity modes in the spectrum play an important role. For an unstratified pool of a highly viscous liquid, the vorticity modes are found to make a large contribution to the temporal evolution of the transient vorticity layer, at the free-surface. It is demonstrated that the temporal evolution of localised vortical perturbations sufficiently deep inside the pool, cannot be captured by surface modes (capillarity-gravity modes) and require contributions from the vorticity modes. The free-surface signature of a deep, localised, vortical perturbation is however found to be negligible. On a stratified pool of viscous liquid, such vortical initial perturbations are shown to have significant projections on vorticity as well as internal gravity modes. In the infinite depth limit of an unstratified pool, the contribution from the continuous spectrum vorticity modes is analysed vis-a-vis that from their finite depth, discrete spectrum counterparts. Several analytical predictions are compared against direct numerical simulations (DNS) obtaining excellent agreement. Our results extend classical ones due to Lamb (1932), Yih (1960), Prosperetti (1976) and Prosperetti and Cortelezzi (1982) and receive support from nonlinear simulations.

Keyword:

Free surface flows

Linear stability analysis

Stratified flows