Forced convection in porous media

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Forced convection is type of heat transport in which fluid motion is generated by an external source like a (pump, fan, suction device, etc.). Heat transfer through porus media is very effective and efficiently. Forced convection heat transfer in a confined porous medium has been a subject of intensive studies during the last decades because of its wide applications.

The basic problem in heat convection through porous media consists of predicting the heat transfer rate between a deferentially heated, solid impermeable surface and a fluid-saturated porous medium. Beginning with constant wall temperature.[1]

In 2D steady state system

u/x+v/y=0

According to Darcy's law

u=(K/μ)P/x

v=(K/μ)P/y

uT/x+vT/y=α2x2T

u=U v=0

P(x)=(μ/K)Ux+constant

δt is the thickness of the slender layer of length x that affects the temperature transition from T0 to T.

Balancing the energy equation between enthalpy flow in the x direction and thermal diffusion in the y direction

UT/xαΔT/δt2

boundary is slender so δt<<x

δt/xPex.5

Nu=hx/Kx/δtPex0.5

The Peclet number is a dimensionless number used in calculations involving convective heat transfer. It is the ratio of the thermal energy convected to the fluid to the thermal energy conducted within the fluid.

Pex = Advective transport rate / Diffusive transport rate

Pex=Ux/α

See also

References

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