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