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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