Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation

The effect of variable gravity on the free convection in a horizontal porous layer with viscous dissipation is investigated. The bottom boundary is taken as adiabatic and there is a non-uniform temperature distribution along the upper boundary. The effect of viscous dissipation is significant and...

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Main Authors: Kamalika Roy, P. V. S. N. Murthy
Format: Article
Language:English
Published: Isfahan University of Technology 2016-01-01
Series:Journal of Applied Fluid Mechanics
Subjects:
Online Access:http://jafmonline.net/JournalArchive/download?file_ID=40919&issue_ID=236
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author Kamalika Roy
P. V. S. N. Murthy
author_facet Kamalika Roy
P. V. S. N. Murthy
author_sort Kamalika Roy
collection DOAJ
description The effect of variable gravity on the free convection in a horizontal porous layer with viscous dissipation is investigated. The bottom boundary is taken as adiabatic and there is a non-uniform temperature distribution along the upper boundary. The effect of viscous dissipation is significant and the top boundary temperature distribution is assumed to have a constant gradient. The gravity varies linearly with the height. A linear stability analysis of the basic flow is carried out. The critical horizontal Rayleigh number is calculated for oblique roll disturbances. The longitudinal rolls are found to be the most unstable ones. The viscous dissipation has a destabilizing effect. There is a drastic decrease in the value of critical horizontal Rayleigh number when modified variable gravity parameter changes from 1 to 1.
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spelling doaj.art-0f538c9a4fdf415da8b882ee2a811d512022-12-22T01:34:49ZengIsfahan University of TechnologyJournal of Applied Fluid Mechanics1735-35722016-01-019526212628.Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous DissipationKamalika Roy0P. V. S. N. Murthy1IIT KharagpurDepartment of mathematics, Indian Institute of Technology Kharagpur, IndiaThe effect of variable gravity on the free convection in a horizontal porous layer with viscous dissipation is investigated. The bottom boundary is taken as adiabatic and there is a non-uniform temperature distribution along the upper boundary. The effect of viscous dissipation is significant and the top boundary temperature distribution is assumed to have a constant gradient. The gravity varies linearly with the height. A linear stability analysis of the basic flow is carried out. The critical horizontal Rayleigh number is calculated for oblique roll disturbances. The longitudinal rolls are found to be the most unstable ones. The viscous dissipation has a destabilizing effect. There is a drastic decrease in the value of critical horizontal Rayleigh number when modified variable gravity parameter changes from 1 to 1.http://jafmonline.net/JournalArchive/download?file_ID=40919&issue_ID=236darcy flow; variable gravity; viscous dissipation.
spellingShingle Kamalika Roy
P. V. S. N. Murthy
Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
Journal of Applied Fluid Mechanics
darcy flow; variable gravity; viscous dissipation.
title Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
title_full Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
title_fullStr Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
title_full_unstemmed Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
title_short Effect of Variable Gravity on Darcy Flow with Impressed Horizontal Gradient and Viscous Dissipation
title_sort effect of variable gravity on darcy flow with impressed horizontal gradient and viscous dissipation
topic darcy flow; variable gravity; viscous dissipation.
url http://jafmonline.net/JournalArchive/download?file_ID=40919&issue_ID=236
work_keys_str_mv AT kamalikaroy effectofvariablegravityondarcyflowwithimpressedhorizontalgradientandviscousdissipation
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