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Convection in a stratified flow in an inclined porous channel - MaRDI portal

Convection in a stratified flow in an inclined porous channel (Q1103485)

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scientific article; zbMATH DE number 4053256
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Convection in a stratified flow in an inclined porous channel
scientific article; zbMATH DE number 4053256

    Statements

    Convection in a stratified flow in an inclined porous channel (English)
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    1988
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    The flow of a fluid of variable viscosity in an inclined channel bounded by two permeable layers is considered. The flow between the permeable layers is governed by Navier-Stokes equations. The flow in the porous medium is governed by Darcy law. The velocity field and the temperature distribution are obtained and the results are discussed.
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    fluid of variable viscosity
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    inclined channel
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    two permeable layers
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    Navier-Stokes equations
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    Darcy law
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    temperature distribution
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