The effect of nonun iform permeability and thermal d iffusivity on natural convection through a porous system heated from the side is investigated numerically. The first part of the study, in Section 2, focuses on systems composed of vert ical sublayers. It is shown that the heattransferrate is infl
Tertiary and quarternary solutions for convection in a vertical fluid layer heated from the side
โ Scribed by R.M. Clever; F.H. Busse
- Publisher
- Elsevier Science
- Year
- 1995
- Tongue
- English
- Weight
- 736 KB
- Volume
- 5
- Category
- Article
- ISSN
- 0960-0779
No coin nor oath required. For personal study only.
โฆ Synopsis
In many fluid systems the evolution from simple to complex forms of flow can be followed through a sequence of supercritical bifurcations. Each of the bifurcations is characterized by the breaking of symmetries and the occupation of new degrees-of-freedom by the fluid motion. The problem of fluid flow in a vertical layer subjected to a horizontal temperature gradient is considered in this paper. The sequence of solutions starts with the cubic profile flow as primary solution, which becomes unstable to steady transverse rolls for Prandtl numbers less than 12.45. A tertiary steady three-dimensional flow in the form of staggered vortices follows, which is replaced by a drifting pattern as the Grashof number is increased even further. It is proposed that the regular periodic solutions are representative for the coherent structures observed in experimental realizations of the problem.
๐ SIMILAR VOLUMES
An analytic technique, namely the homotopy analysis method, is applied to solve the combined heat and mass transfer by natural convection adjacent to a vertical wall in a non-Darcy porous medium governed by a set of three fully coupled, highly nonlinear similarity equations. An explicit, totally ana
A mathematical model is analyzed in order to study the heat and mass transfer characteristics in mixed convection boundary layer flow about a linearly stretching vertical surface in a porous medium filled with a viscoelastic fluid, by taking into account the diffusionthermo (Dufour) and thermal-diff