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...

Full description

Bibliographic Details
Main Author: Singh M.
Format: Article
Language:English
Published: Sciendo 2018-11-01
Series:International Journal of Applied Mechanics and Engineering
Subjects:
Online Access:https://doi.org/10.2478/ijame-2018-0054
id doaj-5e964db6592944bfa4b9b5b76a5da2b0
record_format Article
spelling 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
_version_ 1717781476746985472