Abstract
By substituting the Cattaneo–Christov heat-flow model for the more usual parabolic Fourier law, we consider the impact of hyperbolic heat-flow effects on thermal convection in the classic problem of a magnetized conducting fluid layer heated from below. For stationary convection, the system is equivalent to that studied by Chandrasekhar (
Hydrodynamic and Hydromagnetic Stability,
1961), and with free boundary conditions we recover the classical critical Rayleigh number
R
c
(
c
)
(
Q
)
which exhibits inhibition of convection by the field according to
R
c
(
c
)
→
π
2
Q
as
Q
→
∞
, where
Q
is the Chandrasekhar number. However, for oscillatory convection we find that the critical Rayleigh number
R
c
(
o
)
(
Q
,
P
1
,
P
2
,
C
)
is given by a more complicated function of the thermal Prandtl number
P
1
, magnetic Prandtl number
P
2
and Cattaneo number
C
. To elucidate features of this dependence, we neglect
P
2
(in which case overstability would be classically forbidden), and thereby obtain an expression for the Rayleigh number that is far less strongly inhibited by the field, with limiting behaviour
R
c
(
o
)
→
π
Q
/
C
, as
Q
→
∞
. One consequence of this weaker dependence is that onset of instability occurs as overstability provided
C
exceeds a threshold value
C
T
(
Q
); indeed, crucially we show that when
Q
is large,
C
T
∝
1
/
Q
, meaning that oscillatory modes are preferred even when
C
itself is small. Similar behaviour is demonstrated in the case of fixed boundaries by means of a novel numerical solution.
Subject
General Physics and Astronomy,General Engineering,General Mathematics
Cited by
18 articles.
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