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Free convection from a vertical cylinder embedded in a saturated porous medium

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Summary

The free convection boundary layer on an impermeable vertical cylinder embedded in a saturated porous medium is considered. It is shown that a numerical solution of the governing equations fails to predict the flow at large distances along the cylinder with any real accuracy, though is accurate at moderate distances from the leading edge. An asymptotic solution is derived and it is shown that a simple approximate method can better represent the whole flow region than the full numerical solution.

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Abbreviations

a :

radius of the cylinder

g :

acceleration of gravity

K :

permeability of the porous medium

Q :

non-dimensional heat transfer at the cylinder

g :

wall temperature gradient defined byq=Q/2µ

r :

radial co-ordinate

\(\bar r\) :

non-dimensional radial co-ordinate

R a :

Rayleigh number

T :

temperature of the convective fluid

T w :

temperature of the cylinder

T o :

ambient temperature

ΔT :

temperature difference=T w -T 0

u :

velocity in thex-direction

v :

velocity in ther-direction

x :

axial co-ordinate

X :

non-dimensional axial co-ordinate

α:

equivalent thermal diffusivity

β:

coefficient of thermal expansion

θ:

non-dimensional temperature=(T-T 0)/ΔT

μ:

viscosity of the convective fluid

ϱ:

density of the convective fluid

Ψ:

stream function

µ:

co-ordinate defined by µ=2(2X)1/2

References

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Merkin, J.H. Free convection from a vertical cylinder embedded in a saturated porous medium. Acta Mechanica 62, 19–28 (1986). https://doi.org/10.1007/BF01175850

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  • DOI: https://doi.org/10.1007/BF01175850

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