Environmental Engineering Reference
In-Depth Information
Table 2.4.1
Spectrum of the extraterrestrial solar radiation, (from Petela, 1962).
λ
·
10
10
i
0
,
λ
·
10
−
10
ν
·
10
−
11
i
0
,
ν
·
10
12
λ
·
10
10
ν
·
10
−
12
i
0
,
ν
·
ν
L
0
,
ν
·
10
13
L
0
,
ν
·
ν
W
m
3
sr
1
s
J
m
2
sr
1
s
W
m
2
sr
J
m
2
ssr
W
m
2
Ksr
m
m
1
2
3
4
5
6
7
8
9
2200
2300
2400
.
.
60000
70000
10
26
31
.
.
13627
13035
12492
.
.
15
47
59
100
100
100
62.0
56.7
52.1
.
.
960
2650
3090
.
.
1260
640
0.03
0.10
0.12
.
.
7.19
5.48
0.205
0.540
0.639
.
.
0.514
0.293
.
.
1765
1201
.
.
10000
10000
1
1
500
428
0.714
0.535
Total
10079300
2263.306
Figure 2.4.1
Spectrum of extraterrestrial solar radiation (from Petela, 1962).
The obtained result 1275.8 W/m
2
is the exergy of the extraterrestrial solar
radiation arriving in a 1 m
2
surface which is perpendicular to the direction of
the sun.
The obtained ratio of radiosity (equal to emission) to exergy is
ψ
S
=
1275
.
8
/
1367
.
9
=
0
.
9326.
2.4.1.2 Possibility of concentration of solar radiation exergy
Solar energy, although rich, is poorly concentrated and thus it requires a relatively
large surface to harvest the Sun's radiation. From this viewpoint solar radiation is
especially valuable for those countries which have lot of unused areas (e.g. deserts).
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