Gravity dominated filmcondensation in a porous medium
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Yuwen Zhang (Talk  contribs) 
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[[Image:Gravity_dominated_filmcondensation_on_an_inclined_wall_in_a_porous_medium.pngthumb400 pxalt= Gravity dominated filmcondensation on an inclined wall in a porous medium.  Figure 1 Gravity dominated filmcondensation on an inclined wall in a porous medium.]]  [[Image:Gravity_dominated_filmcondensation_on_an_inclined_wall_in_a_porous_medium.pngthumb400 pxalt= Gravity dominated filmcondensation on an inclined wall in a porous medium.  Figure 1 Gravity dominated filmcondensation on an inclined wall in a porous medium.]]  
  When condensation is dominated by gravity, the effect of surface tension is negligible, and consequently, no twophase region exists. Condensation along an inclined wall in a porous medium (See Fig. 1) will be discussed  +  When condensation is dominated by gravity, the effect of surface tension is negligible, and consequently, no twophase region exists. Condensation along an inclined wall in a porous medium (See Fig. 1) will be discussed here. A porous medium saturated with dry vapor at its saturation temperature, T<sub>sat</sub>, is bounded by an inclined impermeable wall with a temperature T<sub>w</sub> (<math>{{T}_{w}}<{{T}_{sat}}</math>). Since the wall temperature is below saturation temperature, film condensation occurs on the inclined wall and the condensate flows downward due to gravity. It is assumed that the condensation is gravitydominated and, therefore, that the liquid and vapor are separated by a sharp interface, not a twophase region. In addition, the following assumptions are made by [[#ReferencesCheng (1981)]] in order to obtain an analytical solution: 
1. The condensate film is very thin compared to the length of the inclined wall (<math>{{\delta }_{\ell }}\ll L</math>) so that boundary layer  1. The condensate film is very thin compared to the length of the inclined wall (<math>{{\delta }_{\ell }}\ll L</math>) so that boundary layer 
Revision as of 08:12, 26 July 2010
When condensation is dominated by gravity, the effect of surface tension is negligible, and consequently, no twophase region exists. Condensation along an inclined wall in a porous medium (See Fig. 1) will be discussed here. A porous medium saturated with dry vapor at its saturation temperature, T_{sat}, is bounded by an inclined impermeable wall with a temperature T_{w} (T_{w} < T_{sat}). Since the wall temperature is below saturation temperature, film condensation occurs on the inclined wall and the condensate flows downward due to gravity. It is assumed that the condensation is gravitydominated and, therefore, that the liquid and vapor are separated by a sharp interface, not a twophase region. In addition, the following assumptions are made by Cheng (1981) in order to obtain an analytical solution:
1. The condensate film is very thin compared to the length of the inclined wall () so that boundary layer assumption is valid.
2. The properties for the porous medium, liquid, and vapor are independent from temperature.
3. The inclination angle, φ, is small enough for the gravity component in the normal direction of the surface to be negligible.
4. Darcy’s law is valid for both liquid and vapor phases.
5. The saturation temperature, Tsat, is constant.
Under these assumptions, the continuity, momentum, and energy equations for the liquid layer are



The boundary conditions at the wall are


At the interface, the boundary conditions are



where is mass flux of condensate across the interface, and is thermal conductivity of the porous medium saturated with liquid. Combining of eqs. (7) and (8) yields

Introducing stream function

and the following similarity variables:



where

the governing equations and the corresponding boundary conditions become






where

is the dimensionless liquid film thickness and

is Jakob number that measures the degree of subcooling at the wall.
Integrating eq. (15) and considering eq. (17), one obtains

which can be substituted into eqs. (16) and (20) to get


The solution of eq. (24) with eqs. (18) and (19) as boundary conditions is

where the dimensionless film thickness can be obtained by substituting eq. (26) into eq. (25):

The heat flux at the wall is

and the local Nusselt number is

where η_{δ} is function of Jakob number, , as indicated by eq. (27). Cheng (1981) recommended that eq. (29) can be approximated using

In practical application, the average Nusselt number is often of the interest. It can be obtained by integrating eq. (30):

References
Cheng, P., 1981, “Film Condensation Along an Inclined Surface in a Porous Medium,” International Journal of Heat and Mass Transfer, Vol. 24, pp. 983990.
Faghri, A., and Zhang, Y., 2006, Transport Phenomena in Multiphase Systems, Elsevier, Burlington, MA
Faghri, A., Zhang, Y., and Howell, J. R., 2010, Advanced Heat and Mass Transfer, Global Digital Press, Columbia, MO.