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Generalized theoretical framework for spatial attenuation rates of gravity waves in a stepwise-stratified fluid system with multiple layers of arbitrary depths
Phys. Rev. Fluids 10, 054802 – Published 19 May, 2025
DOI: https://doi.org/10.1103/PhysRevFluids.10.054802
Abstract
This study presents a theoretical model for gravity wave attenuation in a multilayered fluid system comprising fluidized mud, water, an interfacial fluid layer (typically enriched with surface-active compounds including oil), and air, which closely mimics the atmosphere-ocean configuration. A rigorous mathematical analysis initiated from the boundary value problem yields the dispersion relation, which is then solved numerically to obtain the complex-valued wave number, whose imaginary part is the spatial attenuation rate. Parametric studies are conducted to investigate how the attenuation rate responds to changes in wave frequencies, fluid and interfacial properties, and layer depths. Results obtained are compared with published experimental data in select cases, showing good agreement. In addition, the model is applied to reduced systems by setting the densities or depths of select layers to zero. For a water-mud system, maximum attenuation rates occur when the mud layer's depth is comparable to the wavelength and exceeds the boundary layer thickness by 100%–200%. Similarly, in an oil-water-mud system, maximum attenuation rates are obtained when the mud layer's depth exceeds the boundary layer thickness by 10%. Further analysis highlights the significance of air dynamics through the ratio, , defined as the attenuation rate in an air-oil-water-mud system relative to that in a corresponding vacuum-oil-water-mud system. Results reveal that for low-frequency waves in deep water systems, with values reaching up to in specific cases. Such high values underscore the critical role of air dynamics in predicting attenuation rates accurately. Moreover, in an air-oil-water-mud system, the maximum value of and the corresponding frequency at which it occurs exhibit power-law dependencies on water layer depth (), scaling as and , respectively. It is inferred that maximum attenuation rates are linked to strong velocity gradients in the fluid layers; they may also be understood by analyzing variations in the group velocity and the penetration depth, which is related to the rotational part of the velocity field.
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