## Abstract Forced convection in channels filled with packed beads with internal heat source was numerically analyzed by using the extended Darcy model for the flow and energy conservation equations with nonthermal equilibrium (NTE). The temperature difference between the matrix and fluid phases wa
Effects of a porous medium on local heat transfer and fluid flow in a forced convection field
โ Scribed by Koichi Ichimiya; Takeshi Matsuda; Yasuyuki Kawai
- Publisher
- Elsevier Science
- Year
- 1997
- Tongue
- English
- Weight
- 595 KB
- Volume
- 40
- Category
- Article
- ISSN
- 0017-9310
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โฆ Synopsis
Abstraet--A numerical estimation was made for the laminar flow and heat transfer through a porous medium placed in a flow passage with a miter bend. Heat transfer between solid material and fluid was considered in the numerical analysis. The calculations were performed for the Darcy number Da = 1-2.5 x 10 -6, ti~e ratio of thermal conductivity of solid material to fluid RRM = 1-1000, the parameter for heat transfer between solid material and fluid H~ = 10--1000 and the Reynolds number Re = 300. The results of local heat transfer and dimensionless stream function were compared for the cases with and without a porous medium. The behavior of the flow, the solid and gas temperatures, the Nusselt number with these parameters and the thermal performance were illustrated. It was found that a porous medium with high RRM and Hs should be selected with an optimum Darcy number to enhance the local heat transfer without a significant flow resistance.
๐ SIMILAR VOLUMES
The convective heat transfer analysis in a channel embedded in a power-law fluid saturated porous medium subject to uniform heat flux is presented and compared with a Newtonian fluid concerning the effects of viscous dissipation. Governing momentum and energy equations for non-Newtonian fluids which
The effects of Hall current and heat transfer on the rotating flow of a second grade fluid past a porous plate with variable suction are examined. The medium considered is porous and suction and external flow velocities vary periodically. The plate is assumed to be at a higher temperature than the f