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
=
Aε
−
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
.
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