Environmental Engineering Reference
In-Depth Information
where ψ is the exergy-energy ratio discussed in paragraph 2.2.5 and the exergy B Q of
heat absorbed by surface A is:
Aq 1
T 0
T
B Q =
(2.4.9)
The reality of the discussed effect of concentration of solar radiation can be eval-
uated by the calculated value of the overall entropy growth , which consists of: the
positive entropies of heat Q , the emission of surface A , and the negative entropy of
absorbed solar radiation:
Q
T +
4
3 σT 3
=
A S εSR
(2.4.10)
where SR is the entropy of irradiance IR . It has to be noted that using the energy
emissivity ε in formula (2.4.10) for entropy calculation is not precise and, as discussed
in details by Petela (2010), the smaller is the precision the smaller is the emissivity
ε . The magnitude SR can be evaluated from the assumed ratio SR / IR to be equal the
ratio s / e of the black emission entropy and emission energy, SR / IR = s / e . With use of
formulae (2.2.32) and (2.2.39), the following relation can be derived:
4
3
IR
T S
SR
=
(2.4.11)
The overall entropy growth determined from equation (2.4.10) should be positive
( > 0). Otherwise, (when
0), the concentration of solar radiation is impossible
as being against the Second Law of Thermodynamics.
Example 2.4.1.3 The concentration of solar radiation can be considered, e.g., at
IR
800 W/m 2
1m 2
=
arriving at the imagined surface of area A S
=
shown in Figure
3 W/(m 2 K) and the environment temperature T 0
2.4.2. Assuming k
300 K equation
(2.4.4) allows for determining the temperature T of surface A as function of the surface
ratio a S . As is shown in Figure 2.4.3, with the increase in a S , the temperature T grows
(thin solid line) and the heat rate q is also increasing (long-dashed line), determined by
formula (2.4.5).
However, according to formula (2.4.6), with growing a S the total heat Q is varying
(short-dash line) with a maximum of about 134 W at about a S
=
=
2. The maximum
appears because with growing a S its effect becomes stronger than the effect of growing
heat rate q .
The energy efficiency η E of concentration of solar radiation, based on definition
(2.4.7) is varying as shown with the thick-dashed line in Figure 2.4.3. The efficiency
η E has the maximum of about 16.8% appearing also at about a S
2, correspondently
to the maximum of Q .
Exergy B Q of absorbed heat is determined by (2.4.9) and shown in Figure 2.4.3
with a dash-dot line. The exergy B Q varies and has a maximum of about 45.8 W, which
appears in the surface area ratio about a S
6. The maximum is a result of two factors
varying with growing a S : one is growing exergy of heat due to growing temperature
T , other is due to diminishing of the absorbed heat Q .
 
Search WWH ::




Custom Search