Physics 103
Home Exercise #2: Solar Energy
Location: You will need to come to Dana 126 in order to check out the experimental equipment. Groups of three are the optimum size (four is the maximum allowed); you need at least one partner. You should do the experiment outside Dana, either on the loading dock on the east end, in the courtyard, or on the street side of the building. The best time to do it is between the hours of 10 am and 3 pm, so that the sun will be more overhead. You need to pick as clear a day as possible. You can use the computers in Dana 126 to analyze your data. I will be glad to answer questions and help you with Excel.
Purpose: To measure the solar insolation reaching the surface of the earth at our location.
Equipment: A black-painted aluminum block mounted in a styrofoam insulation box with a glass cover, a wooden dowel, a thermometer, and a stop watch.
Introduction: The solar insolation (brightness or intensity) at the Earth’s surface is defined as the energy per second that reaches a unit area of surface which is oriented at right angles to the direction of the sunlight. At the top of the earth's atmosphere the insolation is about 1360 W/m2. This value is known as the solar constant. The atmosphere absorbs and reflects roughly one-half of the incident sunlight, so that the insolation that reaches the surface of the earth is about 680 W/m2. The intensity will be different at different latitudes and during the morning or evening when the sun is lower in the sky. Cloud cover will also affect the readings.
You will determine the solar insolation in Davidson, NC on a typical day in the spring. You will measure how the temperature of a black-painted aluminum block increases when it is exposed to the sun. If the black paint is a perfect absorber (a perfect blackbody), then the amount of solar energy incident on the block is equal to the thermal energy absorbed by the block.
Definitions: I = solar insolation
E = energy from the sun incident on the block
Q = gain of thermal energy by the block
A = area of block
T = temperature in ºC
c = specific heat of aluminum = 900 J/kg ºC
t = time
m = mass of aluminum block (on bottom of Styrofoam box)
By definition:
or
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and
,
where D t is the time during which the block is exposed to the sun and D T is the temperature change of the block during that time.
Since
, then
.
We can solve this last equation for the insolation:
.
Thus, your task is to measure the temperature of the aluminum block as a function of time. You can then plot temperature T versus time t on a graph. That graph should be very close to a straight line with slope
ΔT/Δt = rise/run. We can then determine I from the above equation.Procedure:
Data Analysis:
To hand in
We will assume that these two sheets of paper contain the objective, theory and procedure that would normally go into your report. Your report should thus contain a cover page with a title for the exercise, your name, and the names of those with whom you did the exercise. Each person’s report should include a copy of your group’s spreadsheet which includes the data and the graph. You must do your own individual mathematical calculations in the report, with your own result for the insolation identified. You should finish your report with a discussion: a summary of your results and a discussion of why the number may have differed from what you expected, what problems were encountered, and what uncertainties might have influenced your measurements.