
atmospheres, the magnetic field may be variable
and may altogether alter the nature of the
instability. The Coriolis force also plays an
important role on the stability of stellar
atmospheres.
A detailed account of thermal convection, under
varying assumptions of hydrodynamics and
hydromagnetics, has been given by
Chandrasekhar [9]. Veronis [10] has considered
the problem of thermohaline convection in a
layer of fluid heated from below and subjected
to a stable salinity gradient. In the stellar case,
the physics is quite similar to Veronis [10]
thermohaline configuration in that helium acts
like salt in raising the density and in diffusing
more slowly than heat. In thermosolutal-
convective instability problem, buoyancy forces
can arise not only from density differences due
to variations in temperature but also from those
due to variations in solute concentrations. The
conditions under which convective motions are
important in stellar atmospheres are usually far
removed from the consideration of a single
component fluid and rigid boundaries and,
therefore, it is desirable to consider one gas
component acted on by solute concentration
gradient and free boundaries. Marcu and Ballai
[11] have studied the thermosolutal linear
stability of a composite two-component plasma
in the presence of Coriolis forces, finite Larmor
radius, taking into account the collisions
between neutral and ionized particles. The
thermosolutal instability appears due to a
material convection (thermosolutal convection)
in a two component fluid with different
molecular diffusivities which contribute in an
opposing sense to a locally vertical density
gradient. Jamwal and Rana [12] have studied the
magnetohydrodynamic Veronis’s thermohaline
convection.
In recent years, the investigations of flow of
fluids through porous media have become an
important topic due to the recovery of crude oil
from the pores of reservoir rocks. The study of
the onset of convection in a porous medium has
attracted considerable interest because if its
natural occurrence and of its intrinsic
importance in many industrial problems,
particularly in petroleum exploration, chemical,
and nuclear industries. The derivation of the
basic equations of a layer of fluid heated from
below in porous medium, using the Boussinesq
approximation, has been given by Joseph [13].
The study of a layer of fluid heated from below
in porous media is motivated both theoretically
and by its practical applications in engineering
disciplines. Among the applications in
engineering disciplines one can find the food
process industry, chemical process industry,
solidification and centrifugal casting of metals.
The development of geothermal power
resources has increased general interest in the
properties of convection in porous medium.
When a fluid permeates an isotropic and
homogeneous porous medium, the gross effect
is represented by Darcy’s law. A great number
of applications in geophysics may be found in
the books by Phillips [14], Ingham and Pop [15],
and Nield and Bejan [16]. Generally, it is
accepted that comets consist of a dusty
‘snowball’ of a mixture of frozen gases which in
the process of their journey changes from solid
to gas and vice versa. The physical properties of
comets, meteorites, and interplanetary dust
strongly suggest importance of porosity in
astrophysical context (see McDonnel [17]).
Purkayastha and Choudhury [18] have studied
the Hall current and thermal radiation effect on
MHD convection flow of an elastico-viscous
fluid in a rotating porous channel. The porosity
is important in several geophysical situations.
Effects of permeability on double diffusive
MHD mixed convective flow past an inclined
porous plate have been studied by Uddin et al.
[19]. Kumar and Singh [20] have considered the
thermal convection of a plasma in porous
medium to include simultaneously the effect of
rotation and the finiteness of the ion Larmor
radius (FLR) in the presence of a vertical
magnetic field.
Keeping such astrophysical and geophysical
situations in mind, thermal-convective
instability of a composite rotating stellar
atmosphere in the presence of a variable
horizontal magnetic field is considered in the
present paper to include, separately, the effects
of medium permeability and solute gradient.
EARTH SCIENCES AND HUMAN CONSTRUCTIONS
DOI: 10.37394/232024.2022.2.17