Physics:Forced convection in porous media

From HandWiki

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

u∂T/∂x+v∂T/∂y=α∂2∂x2T

u=U∞ v=0

P(x)=−(μ/K)U∞x+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

U∞∂T/∂x∼αΔT/δt2

boundary is slender so δt<<x

δt/x∼Pex−.5

Nu=hx/K∼x/δt∼Pex0.5

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=U∞x/α

See also

References

  1. ↑ Nield, D.A; Bejan, A (2013). Convection in Porous Media. Springer Science & Business Media. ISBN 9780387290966. https://books.google.com/books?id=4qTvIixmtVkC.