Abstract
In this paper we consider the free convection from a horizontal line source of heat which is embedded in an unbounded porous medium saturated with a fluid at rest under gravity. The convective fluid and the porous medium are in local thermal equilibrium.
Zusammenfassung
In dem Aufsatz wird die freie Konvektion von einer horizontalen, linienförmigen Wärmequelle untersucht, die in ein unbegrenztes poröses Medium eingebettet ist. Die Poren des porösen Mediums sind mit einem Fluid gefüllt, das unter Schwerkrafteinfluß ruht. Das strömende Fluid und das poröse Medium sind örtlich im thermischen Gleichgewicht.
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Abbreviations
- c p :
-
specific heat of convective fluid
- F o :
-
parameter,=χα/(vl>g
- g :
-
acceleration due to gravity
- k :
-
thermal conductivity of the saturated porous medium
- l :
-
typical length scale of body
- Q :
-
heat flux per unit length of a line source
- Ra :
-
Rayleigh number, =gβQl/α2μcp
- Ra x :
-
local Rayleigh number, =xg βQx/ a2μcp
- T :
-
temperature
- T ∞ :
-
temperature of ambient fluid
- u, ν :
-
x andy components of velocity
- x, y :
-
coordinates vertically upwards and normal to axis of plume
- X, Y :
-
non-dimensional coordinates vertically upwards and normal to axis of plume
- α :
-
equivalent themal diffusivity
- β :
-
coefficient of thermal expansion
- η :
-
similarity variable
- θ :
-
non-dimensional temperature
- x :
-
permeability of porous medium
- μ :
-
viscosity of convective fluid
- v :
-
kinematic viscosity of convective fluid
- ϱ:
-
density of convective fluid
- ψ :
-
stream function
- Ψ :
-
non-dimensional stream function
- χ :
-
the Forchheimer's coefficient
References
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Cheng, P.: Private communication
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Ingham, D.B. An exact solution for non-darcy free convection from a horizontal line source of heat. Wärme- und Stoffübertragung 22, 125–127 (1988). https://doi.org/10.1007/BF01052976
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DOI: https://doi.org/10.1007/BF01052976