Abstract

Classical Navier–Stokes equations fail to describe some flows in both the compressible and incompressible configurations. In this article, we propose a new methodology based on transforming the fluid mass velocity vector field to obtain a new class of continuum models. We uncover a class of continuum models which we call the re-casted Navier–Stokes. They naturally exhibit the physics of previously proposed models by different authors to substitute the original Navier–Stokes equations. The new models unlike the conventional Navier–Stokes appear as more complete forms of mass diffusion type continuum flow equations. They also form systematically a class of thermo-mechanically consistent hydrodynamic equations via the original equations. The plane wave analysis is performed to check their linear stability under small perturbations, which confirms that all re-casted models are spatially and temporally stable like their classical counterpart. We then use the Rayleigh-Brillouin scattering experiments to demonstrate that the re-casted equations may be better suited for explaining some of the experimental data where original Navier–Stokes equations fail.

Highlights

  • Fluid mechanics is one of the oldest field of science and still widely researched due to its broad spread of applications in many industries [1]

  • An RayleighBrillouin scattering (RBS) spectrum typically consists of a central Rayleigh peak near fs = 0 and two Brillouin side peaks at an equidistance from the central Rayleigh peak

  • In the typical spectra of the coherent RBS, one can notice the presence of Brillouin peaks only when the gas flow is in the hydrodynamic regime (Kn ≤ 0.001)

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Summary

Introduction

Fluid mechanics is one of the oldest field of science and still widely researched due to its broad spread of applications in many industries [1]. The development of basic fundamental dynamic laws such as Newton’s law of motion and Newton’s law of viscosity culminated in the current form of the Navier-Stokes equations; these equations are still widely accepted as the universal basis of modelling fluid motion [2, 3]. They are frequently solved by using numerical computational methods. Improving the range of applicability of the Navier-Stokes equations beyond their limits has been and still is a critical area of research

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