HYDRODYNAMIC INSTABILITY IN A POROUS LAYER SATURATED WITH A HEAT GENERATING FLUID.

F. A. KULACKI; R. RAMCHANDANI

HYDRODYNAMIC INSTABILITY IN A POROUS LAYER SATURATED WITH A HEAT GENERATING FLUID.

F. A. KULACKI
, R. RAMCHANDANI

Mechanical Engineering

Research output: Contribution to journal › Article › peer-review

Abstract

Critical Rayleigh numbers determined by linear stability theory are presented for porous-fluid layers of infinite horizontal extent heated internally by a uniform volumetric energy source in the fluid. The thermal coupling between the layer and its environment is represented by a general mixed boundary condition for both the conduction state and the disturbance temperature. Rigid-rigid, rigid-constant pressure, and constant pressure-rigid boundaries are considered in the computations.

Original language	English (US)
Pages (from-to)	179-185
Number of pages	7
Journal	Heat and Mass Transfer
Volume	8
Issue number	3
State	Published - Dec 1 1975

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title = "HYDRODYNAMIC INSTABILITY IN A POROUS LAYER SATURATED WITH A HEAT GENERATING FLUID.",

abstract = "Critical Rayleigh numbers determined by linear stability theory are presented for porous-fluid layers of infinite horizontal extent heated internally by a uniform volumetric energy source in the fluid. The thermal coupling between the layer and its environment is represented by a general mixed boundary condition for both the conduction state and the disturbance temperature. Rigid-rigid, rigid-constant pressure, and constant pressure-rigid boundaries are considered in the computations.",

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Y1 - 1975/12/1

N2 - Critical Rayleigh numbers determined by linear stability theory are presented for porous-fluid layers of infinite horizontal extent heated internally by a uniform volumetric energy source in the fluid. The thermal coupling between the layer and its environment is represented by a general mixed boundary condition for both the conduction state and the disturbance temperature. Rigid-rigid, rigid-constant pressure, and constant pressure-rigid boundaries are considered in the computations.

AB - Critical Rayleigh numbers determined by linear stability theory are presented for porous-fluid layers of infinite horizontal extent heated internally by a uniform volumetric energy source in the fluid. The thermal coupling between the layer and its environment is represented by a general mixed boundary condition for both the conduction state and the disturbance temperature. Rigid-rigid, rigid-constant pressure, and constant pressure-rigid boundaries are considered in the computations.

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M3 - Article

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IS - 3

ER -

HYDRODYNAMIC INSTABILITY IN A POROUS LAYER SATURATED WITH A HEAT GENERATING FLUID.

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