scispace - formally typeset
Journal ArticleDOI

On the effect of porous thick horizontal partial partition attached to one of the active walls of a differentially heated square cavity

TLDR
In this article, the effect of a horizontal partial porous partition on heat transfer and flow structure in a differentially heated square cavity is investigated, where the fluid flow is assumed to be governed by Navier-Stokes equations and fluid saturated porous media is governed by Darcy's equations.
Abstract
The effect of a horizontal partial porous partition on heat transfer and flow structure in a differentially heated square cavity is investigated. While the fluid flow is assumed to be governed by Navier—Stokes equations, fluid saturated porous media is assumed to be governed by Darcy’s equations. Standard Galerkin method of finite element formulation is applied for discretization of the system of equations. The non‐linearities in the discretized equations are treated with Newton‐Raphson scheme. The code developed is tested for validation for modified Rayleigh number Ra up to 400. The code is then applied to a differentially heated square cavity with a horizontal partial porous partition. While the thickness of the porous partition is found to have appreciable effect on heat transfer and flow field, width of the porous partition is found to have insignificant bearing on heat transfer except when the partition is very small and compatible to the thickness of the boundary layer developed. During the experime...

read more

Citations
More filters
Journal ArticleDOI

Conjugate natural convection heat transfer in an open-ended square cavity partially filled with porous media

TL;DR: In this article, a new lattice Boltzmann (LB) approach was developed to overcome the difficulty of conjugate problems on fluid-porous interfaces, which is validated by three benchmark tests.
Journal ArticleDOI

Upward and downward conjugate mixed convection heat transfer in a partially porous cavity

TL;DR: In this article, the authors provided a numerical study of conjugate heat transfer by mixed convection and conduction in a lid-driven enclosure with thick vertical porous layer, and the effect of the relevant parameters: Richardson number (Ri=0.1, 1, 10, 100) and thermal conductivity ratio (Rk = 0.
Journal ArticleDOI

Minimization of exergy destruction with discrete metal foam filling in a pipe under turbulent flow condition

TL;DR: In this paper , the authors presented the numerical analysis of exergy transfer and irreversibility through the discrete filling of high-porosity aluminum metal foams inside the horizontal pipe.
References
More filters
Journal ArticleDOI

Convection in a porous layer

TL;DR: In this paper, the boundary-layer structure on the side walls of a rectangular cavity filled with a porous material is determined using an integral relations approach, which leads to results for the core mass flux, for core-temperature gradient and for the heat transfer characteristics which are in excellent agreement with numerical solutions of the boundary layer equations.
Journal ArticleDOI

Numerical Study of High Rayleigh Number Convection in a Vertical Porous Enclosure

TL;DR: The results of a numerical simulation of natural convection in a vertical rectangular porous enclosure subjected to a horizontal temperature differential are presented in this paper, which provides a clear physical picture of the development process as R is increased toward asymptotically high values (R →).
Journal ArticleDOI

Natural Convection in a Vertical Enclosure With Internal Permeable Screen

TL;DR: In this paper, the thermal insulation effect of a screen installed inside a vertical rectangular enclosure (e.g., double-glazed window) is investigated. But the focus is on the closed position, where the strips almost touch.

TRANSIENT EFFECTS IN GEOTHERMAL CONVECTIVE SYSTEMS A thesis submitted in partial fulfilment of the requirements of the degree of Doctor of Philosophy at the University of Auckland

TL;DR: In this article, a detailed analysis of the transient behaviour of geothermal convective systems is presented, where the flow in these systems is found to be fluctuating or regular oscillatory in a simplified two-dimensional model and these unsteady effects persist when the model is refined to include the concepts of temperature dependent viscosity and fluid withdrawal and recharge.
Related Papers (5)