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Experimental and Numerical Analysis of a PCM-Supported ...

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the viscous transport <strong>and</strong> introduces velocities in special directions as dependent<br />

variables. The flow field can be determined by solving the Brinkman equation for the<br />

momentum balance in combination with the continuity equation. Applying Brinkman<br />

equation on two phase flow by using the relative permeability K r , the gas phase<br />

momentum balance equation reads:<br />

vg<br />

)<br />

t<br />

<br />

g<br />

( p<br />

g vg<br />

gvg<br />

(4.30)<br />

KK<br />

rg<br />

where μ is the dynamic viscosity, K is the permeability, p<br />

is the pressure gradient,<br />

<strong>and</strong> ρ is the varying gas density. The buoyant force appears automatically when an<br />

equation <strong>of</strong> state is inserted into the equation <strong>of</strong> motion (4.30) in the (ρg) term (but<br />

not into the acceleration term ( v t<br />

)).<br />

v<br />

<br />

t<br />

rel,<br />

g<br />

<br />

T<br />

T <br />

c<br />

c <br />

g<br />

( p<br />

<br />

ref<br />

g)<br />

vg<br />

gvg<br />

<br />

ref<br />

g t<br />

ref c ref<br />

(4.31)<br />

KK<br />

The form <strong>of</strong> equation (4.31) is similar to the Boussinesq equation for forced <strong>and</strong> free<br />

convection in non-isothermal flow in free (non-porous media) flow when the second<br />

<strong>and</strong> third term on the right h<strong>and</strong> side can be omitted. Therefore, this form <strong>of</strong> the<br />

equation <strong>of</strong> motion is very useful for heat <strong>and</strong> mass transfer analysis. For forced<br />

convection the buoyant term g<br />

T<br />

T<br />

<br />

c<br />

c <br />

ref<br />

t<br />

ref<br />

c<br />

ref<br />

, which represents the<br />

momentum transfer caused by the combined buoyancy forces, can be neglected<br />

while for free convection the term ( p<br />

g)<br />

is small <strong>and</strong> omitting it is usually<br />

appropriate [19]. It is also customary [19] to replace ρ on the left side <strong>of</strong> equation<br />

(4.31) by the gas density at inlet conditions. This substitution has been successful for<br />

free convection at moderate temperature differences. Under these conditions the<br />

fluid motion is slow, <strong>and</strong> the acceleration term v t<br />

is small compared to g [19].<br />

4.2.2.2 Flow in the condenser<br />

Figure 4.5a shows the physical system <strong>of</strong> direct contact condensation in the <strong>PCM</strong><br />

condenser. Figure 4.5b shows a schematic illustration <strong>of</strong> energy <strong>and</strong> mass flow in a<br />

rectangular finite element <strong>of</strong> the packed bed. Comparing figure (4.5) <strong>and</strong> figure (4.4),<br />

due to similarity between the evaporator <strong>and</strong> condenser designs, a similar set <strong>of</strong><br />

coupled partial differential equations (4.11) – (4.18) as well as other state variable<br />

equations are found to represent heat <strong>and</strong> mass balances for the condenser.<br />

Altering the signs <strong>of</strong> the last two terms in both equations (4.12) <strong>and</strong> (4.13), the same<br />

form <strong>of</strong> the energy <strong>and</strong> mass balance equations could be applied on the<br />

condensation bed, with some modifications to take into account the condensation on<br />

the solid surface that might take place in parallel with the absorption <strong>of</strong> water vapor<br />

ref<br />

77

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