Bài giảng Green energy course syllabus - Chapter 4: Solar resource - PV materials - Nguyễn Hữu Phúc

Green Energy Course-  
Renewable Energy Systems  
Biên sọan: Nguyễn Hữu Phúc  
Khoa Điện- Điện Tử- Đại Học Bách Khoa TPHCM  
The Solar Resource  
• Before we can talk about solar power, we need to talk  
about the sun  
• Need to know how much sunlight is available  
• Can predict where the sun is at any time  
• Insolation : incident solar radiation  
• Want to determine the average daily insolation at a site  
• Want to be able to chose effective locations and panel  
tilts of solar panels  
The Sun and Blackbody Radiation  
• The sun  
– 1.4 million km in diameter  
– 3.8 x 1020 MW of radiated electromagnetic energy  
• Blackbodies  
– Both a perfect emitter and a perfect absorber  
– Perfect emitter – radiates more energy per unit of surface area  
than a real object of the same temperature  
– Perfect absorber – absorbs all radiation, none is reflected  
The Solar Resource  
• Before we can talk about solar power, we need to talk  
about the sun  
• Need to know how much sunlight is available  
• Can predict where the sun is at any time  
• Insolation : incident solar radiation  
• Want to determine the average daily insolation at a site  
• Want to be able to chose effective locations and panel  
tilts of solar panels  
Plank’s Law  
• Plank’s law – wavelengths emitted by a blackbody  
depend on temperature  
3.74108  
E  
(7.1)  
14400   
5 exp  
1  
T  
• λ = wavelength (μm)  
• Eλ = emissive power per unit area of blackbody  
(W/m2-μm)  
• T = absolute temperature (K)  
Electromagnetic Spectrum  
Visible light has a wavelength of between 0.4 and 0.7 μm, with  
ultraviolet values immediately shorter, and infrared immediately longer  
Source: en.wikipedia.org/wiki/Electromagnetic_radiation  
288 K Blackbody Spectrum  
The earth as a blackbody  
Figure 7.1  
Area under curve is the total radiant power emitted  
Stefan-Boltzmann Law  
• Total radiant power emitted is given by the Stefan –  
Boltzman law of radiation  
E AT 4  
(7.2)  
• E = total blackbody emission rate (W)  
• σ = Stefan-Boltzmann constant = 5.67x10-8 W/m2-K4  
• T = absolute temperature (K)  
• A = surface area of blackbody (m2)  
Wien’s Displacement Rule  
• The wavelength at which the emissive power per unit  
area reaches its maximum point  
2898  
max   
(7.3)  
T
• T = absolute temperature (K)  
• λ = wavelength (μm)  
• λmax =0.5 μm for the sun , T = 5800 K  
• λmax = 10.1 μm for the earth (as a blackbody), T = 288 K  
Extraterrestrial Solar Spectrum  
Figure 7.2  
Air Mass Ratio  
As sunlight passes through the  
atmosphere, less energy arrives at the  
earth’s surface  
Figure 7.3  
• h1 = path length through atmosphere with sun directly  
overhead  
• h2 = path length through atmosphere to spot on surface  
• β = altitude angle of the sun  
Air Mass Ratio  
h2 1  
air mass ratio m =  
h sin  
(7.4)  
1
Figure 7.3  
• Air mass ratio of 1 (“AM1”) means sun is directly  
overhead  
• AM0 means no atmosphere  
• AM1.5 is assumed average at the earth’s surface  
Solar Spectrum on Surface  
M increases  
as the sun  
appears  
lower in  
the sky. Notice  
there is  
a large loss  
towards the blue  
end for higher m,  
which is why the  
sun appears  
reddish at sun  
rise and sun set  
ECE 333 (398RES)  
Renewable Energy Systems  
Lecture 23  
The Solar Resource  
Professor Tom Overbye  
Department of Electrical and  
Computer Engineering  
Announcements  
• Homework 11 is 7.3, 7.14 (use approximation equations  
given in book rather than table data), 7.15, 7.17. It is due  
on Thursday April 30.  
• Reading: Chapters 7 and 8  
• Final exam is on Friday May 8 from 8 to 11am. Because  
of the class size we have two rooms, 106B8 Eng. Hall and  
163 Everitt.  
– Last name starting with A through J go to 163, otherwise 106B8.  
– Final is comprehensive, with more emphasis on solar (since it  
wasn’t on an earlier exam)  
– Same procedure except you can bring in one new notesheet and  
your two previous notesheets.  
Another Projection on How Quickly  
Our Resources will Vanish  
However New Reserves and Sources  
Often Appear: Uranium Example  
• Chart shows uranium resources at 59 years at current  
production levels.  
• In 2006 worldwide production of uranium ore was  
about 40,000 tonnes. Economicially viable reserves  
now at about 5.5 million tonnes, a value that has  
recently increased because of the increase in price.  
• There are estimated to be 35 million tonnes than could  
eventually be mined economically.  
• Uranium can be extracted from sea water giving an  
ultimate potential of about 4.6 billion tonnes, enough  
for 100,000 years at the current rate of consumption.  
Solar Spectrum on Surface  
M increases  
as the sun  
appears  
lower in  
the sky. Notice  
there is  
a large loss  
towards the blue  
end for higher m,  
which is why the  
sun appears  
reddish at sun  
rise and sun set  
In the News: Solar for Chicago  
• On 4/22/09 Exelon announced plans to build a solar  
power plant on Chicago’s South Side.  
• The $60 million solar power plant will provide a  
maximum of about 10MW. Exelon will be relying on  
loan guarantees from the US DOE as part of the  
economic stimulus plan  
• The solar plant will be located in the West Pullman  
neighborhood  
• Assuming a 25% capacity factor, a zero percent interest  
rate, $0.15 electricity, payback time on the plant will be  
$60,000,000/(0.15*8760*10,000*0.25) = 18.3 years  
The Earth’s Orbit  
• One revolution every 365.25 days  
• Distance of the earth from the sun  
360(n 93)  
d 1.5108 10.017sin  
km (7.5)  
365  
• n = day number (Jan. 1 is day 1)  
• d (km) varies from 147x106 km on Jan. 2 to 152x106  
km on July 3 (closer in winter, further in summer)  
• Note that the angles in this chapter are in degrees  
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