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Published byClaude Tate Modified over 8 years ago
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SOLAR ENERGY I
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Solar Energy is an Energy Flow 1 kW∙hr = 3.6 x 10 6 J 1 BTU = 1055.06 J
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What do you consider to be solar energy? A.Photovoltaics B.Wind C.Hydroelectric dams D.Biofuels E.Solar collectors F.All of the above
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Solar Energy is an Energy Flow Many different forms of energy ultimately come from solar Solar heating Photovoltaic Wind Hydroelectric Biomass OTEC Other?
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Should you be allowed to install solar energy units on your property? A.Yes B.No
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Should new construction be required to incorporate energy? A.Yes B.No
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Breakdown of Solar Energy
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How Much Energy is Available? Solar constant is 1368 W/m 2 or 2(cal/min)/cm 2. When averaging over the whole planet, reduce by ½ because half of earth is night, reduce by another ½ because earth is curved. (This is still at top of atmosphere.)
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Approximately 49% of the sunlight at the top of the atmosphere is absorbed by the surface. (We’ll usually assume 50%)
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Power Density at the Surface Average energy at the surface has been reduced by a factor of 8. Average power over the entire planet is approximately 170 W/m 2 or 0.25(cal/min)/cm 2 The power density depends on where you are, but this is a global average.
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Average Energy Density for a Full Day 170W/m 2 ×24 hr=4.08 kWhr/m 2. Solar Insolation: Amount of solar radiation reaching the earth’s surface. Solar insolation varies with time of day, time of year, location on earth, weather.
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Solar Insolation at 40 N Latitude
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Total Solar Energy in US. If we sum the total solar insolation over the entire US we receive approximately 5.610 19 Btu/year. We use approximately 110 17 Btu of energy per year. Thus, we get around 525 times more energy from the sun than we use every year. If we had 100% efficient solar collectors, we could run the country and still only cover 0.16% with solar collectors!
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Solar Heating Active systems: use pumps or fans to move air or a fluid around Have moving parts Consume energy Passive systems: have no moving parts or power use Rely on absorption of energy in mass, density differences, or natural windflow
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Solar Heating: Active system Fluid is forced through a collector by a pump or blower.
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Advantages of active systems Compact components Flexibility of placement/storage units Easy to control. Disadvantages: Requires power to operate it Has moving parts
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Active Solar Collectors
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Selecting the proper angle is important for optimal collection For a fixed panel, make sure it points south (in the Northern Hemisphere.)
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What should the angle be for June? A.18.4º B.71.6º C.47.1º D.45º
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Increased Solar Collection by proper tilting of panel.
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Solar Heating: Passive System Use natural convection currents and architectural features to circulate heat: No external energy required, but very little flexibility.
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Examples of Passive Solar Elements Trombe Wall
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Roof overhang and thermal mass flooring/walls
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Room Arrangement
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Natural Ventilation
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Insulation Reduce the flow of energy into/out of house. Reduce air infiltration by sealing cracks About 50% of energy loss through infiltration
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Heating Degree Days: In general, no additional heat is required if T avg > 65F. T avg = (T high + T low )/2 Definition:Heating Degree Day (HDD) = 65-T avg Often for some time period (like 30 days, or a year)
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If T avg is 15F how many HDD? A.15 B.65 C.50 D.80
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Average HDD for US.
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Insulation: The amount of insulation used in construction depends on the expected number of HDD in a given region. Measured in terms of R value, R is the thermal resistance. (Recall conduction discussion)
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How much heat energy do we need? Need to replace heat lost through walls, roof, etc.
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Example of Heat requirements Consider a 1000 ft 2 house in a 6000 HDD area, insulated to R-15 What heat will be lost through the walls?
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Example of Heat requirements Consider a 1000 ft 2 house in a 6000 HDD area, insulated to R-15 What heat will be lost through the walls? Each wall is (roughly) 32 ft x 10 ft
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Heat lost through walls A.115 MBtu B.2764 MBtu C.12.3 MBtu D.184 MBtu
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Example of Heat requirements
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