Abstract

The study was performed to analyze the flux of energy of internal gravitational-capillary waves in a two-layer hydrodynamic liquid system with finite layer thicknesses. The problem was considered for an ideal incompressible fluid in the field of gravity as well as taking into account the forces of surface tension. The problem was formulated in a dimensionless form for small values of the coefficient of nonlinearity. The dispersion of the gravitational-capillary progressive waves was studied in detail depending on the coefficient of surface tension and the ratio of layer densities. It was proved that with the increase in the wavenumber, the group velocity begins to pass ahead of the phase velocity and their equality occurs at the minimum of the phase velocity. Dependence of the total average energy flux on the wavenumber (wavelength) and thickness of the liquid layers was calculated and graphically analyzed for different values of physical quantities, in particular, density and the coefficient of surface tension. It follows from the analysis that the energy flux of gravitational internal waves increases to a certain maximum value with an increase in the thickness of the lower layer and then approaches a certain limit value. For capillary waves, the energy flux of internal waves is almost independent of the thickness of the lower layer. It was also shown that the average energy flux for gravitational waves at a stable amplitude is almost independent of the wavelength. On the contrary, for capillary waves, the energy flux increases sharply with an increase in the wavenumber. The results of the analysis of the energy flux of internal progressive waves make it possible to qualitatively assess physical characteristics in the development of environmental technologies that use internal undulatory motions in various aquatic environments as a source of energy

Highlights

  • Internal waves are undulatory motions in a stratified fluid

  • The results show that vortex processes energetically dominate in the energy flux of the internal wave in this range of parameters

  • The data obtained in the study of the problem of propagation of internal wave energy in a liquid three-layer hydrodynamic system can be used in the study of similar ocean areas

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Summary

Introduction

Internal waves are undulatory motions in a stratified fluid. Stratification means that, for example, ocean water is divided into layers of different densities which increase with depth. Stratification is caused by various natural phenomena: storms, melting of ice, heating of upper water layers, changes in ocean salinity, etc. It is at the boundary of layers with different densities that a whole class of different wave phenomena occurs. The relevance of studying such phenomena is determined by the necessity of developing environmental technologies that use internal waves as a source of energy in various aquatic environments. Such a study will be useful in creating devices for damping internal waves where they are harmful. Growth or reduction of energy flux of internal waves creates a significant impact on natural processes in water bodies

Literature review and problem statement
The aim and objectives of the study
Phase and group velocities of progressive internal waves
Conclusions
Full Text
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