Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium
An investigation made on the effect of Hall currents on double-diffusive convection of a compressible synovial (couple-stress) fluid in the presence of a horizontal magnetic field through a porous layer is considered. The analysis is carried out within the framework of linear stability theory and no...
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Online Access: | https://doi.org/10.2478/ijame-2018-0054 |
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doaj-5e964db6592944bfa4b9b5b76a5da2b02021-09-05T21:02:02ZengSciendoInternational Journal of Applied Mechanics and Engineering1734-44922353-90032018-11-0123496397610.2478/ijame-2018-0054ijame-2018-0054Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous MediumSingh M.0Department of Mathematics, Govt PG College Seema (Rohru), Distt Shimla (H.P)-171207, IndiaAn investigation made on the effect of Hall currents on double-diffusive convection of a compressible synovial (couple-stress) fluid in the presence of a horizontal magnetic field through a porous layer is considered. The analysis is carried out within the framework of linear stability theory and normal mode technique. A dispersion relation governing the effects of viscoelasticity, compressibility, magnetic field and porous layer is derived. For the stationary convection, a synovial fluid behaves like an ordinary Newtonian fluid due to the vanishing of the viscoelastic parameter. The stable-solute gradient, compressibility, and magnetic field have postponed the onset of convection, whereas Hall currents and medium permeability have not postponed the onset of convection, moreover, a synovial fluid has a dual character in the presence of Hall currents, whereas in the absence of Hall current in synovial fluid have postponed the onset of convection, which is in contrast in case of thermal convection couple-stress fluid with same effects. These analytic results are confirmed numerically and the effects of various parameters are depicted graphically. It has been observed that oscillatory modes are introduced due to the presence of viscoelasticity, magnetic field, porous medium and Hall currents which were non- existent in their absence. The sufficient conditions for the non-existence of overstability are also obtained.https://doi.org/10.2478/ijame-2018-0054compressibilitysynovial fluiddouble-diffusive convectionporous medium and hall current76a0576a1076d5076e0676e1576e0776e1776e1976n2076u0576w0580a20 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Singh M. |
spellingShingle |
Singh M. Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium International Journal of Applied Mechanics and Engineering compressibility synovial fluid double-diffusive convection porous medium and hall current 76a05 76a10 76d50 76e06 76e15 76e07 76e17 76e19 76n20 76u05 76w05 80a20 |
author_facet |
Singh M. |
author_sort |
Singh M. |
title |
Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium |
title_short |
Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium |
title_full |
Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium |
title_fullStr |
Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium |
title_full_unstemmed |
Double-Diffusive Convection of Synovial (Couple-Stress) Fluid in the Presence of Hall Current Through a Porous Medium |
title_sort |
double-diffusive convection of synovial (couple-stress) fluid in the presence of hall current through a porous medium |
publisher |
Sciendo |
series |
International Journal of Applied Mechanics and Engineering |
issn |
1734-4492 2353-9003 |
publishDate |
2018-11-01 |
description |
An investigation made on the effect of Hall currents on double-diffusive convection of a compressible synovial (couple-stress) fluid in the presence of a horizontal magnetic field through a porous layer is considered. The analysis is carried out within the framework of linear stability theory and normal mode technique. A dispersion relation governing the effects of viscoelasticity, compressibility, magnetic field and porous layer is derived. For the stationary convection, a synovial fluid behaves like an ordinary Newtonian fluid due to the vanishing of the viscoelastic parameter. The stable-solute gradient, compressibility, and magnetic field have postponed the onset of convection, whereas Hall currents and medium permeability have not postponed the onset of convection, moreover, a synovial fluid has a dual character in the presence of Hall currents, whereas in the absence of Hall current in synovial fluid have postponed the onset of convection, which is in contrast in case of thermal convection couple-stress fluid with same effects. These analytic results are confirmed numerically and the effects of various parameters are depicted graphically. It has been observed that oscillatory modes are introduced due to the presence of viscoelasticity, magnetic field, porous medium and Hall currents which were non- existent in their absence. The sufficient conditions for the non-existence of overstability are also obtained. |
topic |
compressibility synovial fluid double-diffusive convection porous medium and hall current 76a05 76a10 76d50 76e06 76e15 76e07 76e17 76e19 76n20 76u05 76w05 80a20 |
url |
https://doi.org/10.2478/ijame-2018-0054 |
work_keys_str_mv |
AT singhm doublediffusiveconvectionofsynovialcouplestressfluidinthepresenceofhallcurrentthroughaporousmedium |
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1717781476746985472 |