On the Effects of Magnetic Field and
Temperature-Dependent Viscosity on the Onset Magnetoconvection
for General Boundary Conditions
Joginder Singh Dhiman and
Vijay Kumar
Department of Mathematics,
Himachal Pradesh University, Summerhill, Shimla (H.P.)-171005.
*Corresponding Author: jsdhiman66@gmail.com
ABSTRACT:
In the present paper, the problem of thermal instability
of an electrically conducting fluid layer heated from below and permeated with
a uniform vertical magnetic field is studied for all combinations of rigid and
dynamically free boundary conditions. The effect of temperature-dependent
viscosity on the onset of hydromagnetic thermal
convection is investigated both analytically and numerically. The validity of
the principle of exchange of stabilities for this general problem has been
investigated using the Pellew and Southwell’s
method and a sufficient condition for the validity of this principle is also
derived. The values of the Rayleigh numbers for each case of boundary
combinations are obtained numerically using Galerkin
technique. Further, the effect of temperature-dependent viscosity on the onset
of stationary convection and consequently on the celebrated
1. INTRODUCTION:
The hydrodynamic
stability has been recognized as one of the central problems of fluid
mechanics. It is concerned with when and how laminar flows break down, their
subsequent development and their eventual transition to turbulence. It has many
applications in engineering, meteorology, oceanography, astrophysics and
geophysics. The hydrodynamic thermal instability or thermal convection in a
plane horizontal fluid layer heated from below (also known as Rayleigh–Bénard convection) is a type of convection considered most
frequently. In this phenomenon, spatial and temporal effects are largely
decomposed because of the lack of intense streams determined by external
conditions. For this reason, both the experimental and theoretical treatment of
the Rayleigh–Bénard convection proves to be
especially fruitful. For broad view of the subject of Rayleigh-Bénard convection, one may be referred to Jeffrey’s [1928],
Low [1929], Pellew and Southwell
[1940] and Chandrasekhar [1961].
The hydromagnetic
stability or magnetoconvection is the study of the
effect of an externally impressed magnetic field on the onset of thermal
instability in electrically conducting fluids. In broad terms, the subject of hydromagnetics is concerned with the ways in which magnetic
fields can affect fluid behavior. The problem of thermal instability in the
presence of a magnetic field illustrates many general principles of the
subject.
Recent
developments in astrophysics and geophysics have widespread interest in magnetoconvection because the magnetic fields are believed
to be driven by buoyancy forces. The studies pertaining to magnetoconvection
are extensively investigated over the years, and is well established fact that
the effect of magnetic field is to make the system more stable.
Chandrasekhar
[1961] studied the magnetoconvective instability
problems in detail and laid some guiding principles for the onset of magnetoconvection. He
studied the magnetoconvection in detail and due to
the mathematical complexity involved in solving equations, a very few exact
solutions of the problem exist in literature. He proved his famous
It is well known fact that the viscosity is one of the properties of a
fluid which are most sensitive to temperature (c.f. Straughan
[2002], Kumar V. [2012]). In the majority of the cases, viscosity
becomes the only property which may have considerable effect on the heat
transfer, whereas the temperature variation and dependence of other
thermo-physical properties to temperature are often negligible. Hence, the variation in viscosity behaviour with temperature may have a pronounced effect on
the convective motions of the fluid.
Motivated by the above discussions, the present study is concerned with
buoyancy driven magneto convection in an electrically conducting fluid layer heated from below for which the viscosity of the fluid may
depend strongly on the local temperature. The problem of thermal
instability of an electrically conducting fluid layer heated from below and
permeated with a uniform vertical magnetic field is studied for all
combinations of rigid and dynamically free boundary conditions, and the effect
of temperature-dependent viscosity on the onset of hydromagnetic
thermal convection is investigated both analytically and numerically. The validity of the principle of exchange of stabilities (PES)
for this general problem has been investigated using the Pellew
and Southwell’s method, since
the establishment of PES implies the non-occurrence of any slow oscillatory
motions which may be neutral or unstable. Further, a sufficient condition for
the validity of PES is also derived. The expressions for the Rayleigh numbers
for each case of boundary combinations are obtained numerically using Galerkin technique and the values of each expression is
computed numerically. The effects of temperature-dependent viscosity and
Chandrasekhar number
5. REFERENCE:
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Banerjee, M. B., Shandil, R.G. and
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Received on 12.01.2013 Accepted on 08.02.2013
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Research J. Science and Tech 5(1): Jan.-Mar.2013 page 104-109