Harvard-Westlake School
Show all pertinent measurements, conversion factors and calculations if you would like to earn full credit for this assignment
For the month of January, 1997, Harvard-Westlake purchased 490,900 cubic feet of natural gas to heat the pool.
1. The heat in one cubic foot of gas is 1,021 BTUs. How much heat was purchased?
2. A British Thermal Unit (BTU) is the amount of energy required to heat one pound of water 1°F. Also, it is equivalent to 252 calories. One calorie is the amount of energy required to heat 1 gram of water 1°C. The Harvard-Westlake pool holds 325,000 gallons of water. One gallon of water weighs 8 pounds. Determine the number of pounds of water in the Harvard-Westlake pool.
3. If the conversion of natural gas to heat in the pool were 100% efficient, what change in temperature would be produced?
4. The pool is kept at 80°F and the average temperature during January is 58°F. How much energy is needed to raise the temperature of the pool?
5. How much heat is lost in the conversion from chemical energy to heat in the pool?
6. What is the efficiency of heating the pool?
7. The gas furnace is 80% efficient at converting gas energy to thermal energy in the water. How much energy is initially absorbed by the water?__________
8. Heat is lost from the water to the air, despite the fact that the pool cover is employed most of the day. What is the efficiency of the pool cover? Hint: if the cover was 100% efficient, all of the energy initially absorbed by the water would be retained, but it’s not….
R-Value Worksheet
One of the most economical ways to reduce heat loss or gain in buildings is by using appropriate insulation during construction or by retrofitting afterwards. Most insulating materials are rated as to their insulating effectiveness by a unit called an R-value, which indicates a materials resistance to the flow of heat through it. 1/R is a measure of the amount of heat energy (in British Thermal Units) that would pass through a piece of material 1 square foot in area in 1 hour when the temperature is 1 degree Fahrenheit higher on one side of the material than on the other. If very little heat flowed from one area to the other, then the material between the areas would be a good insulator, for it would have a large R-value. One way to represent the relationship is:
1 = Heat(BTUs)______ or R = Area(ft2) t(F) time (hour)
R Area(ft2) t(F) time (hour) Heat (BTU)
British Thermal Units are usually abbreviated to BTUs, and are equal to the amount of heat energy necessary to raise one pound of water 1 degree F ( or = 252 calories = 1056 joules = 1.056 kilojoules)
Using the same formula, you can determine the amount of heat that has passed through a barrier by
Heat (BTU) = Area(ft2) t(F) time (hour
R
BTUs in various fuels
1 gallon of fuel oil: 145,000
1 gallon of gasoline: 125,000
1 cubic foot of natural gas; 1031
1 ton of coal: 25,000,000
1 cord of wood: 20,000,000
1kWh = 3413 BTU
1. An R-value measuring apparatus maintains a one degree F difference between two compartments separated by a single pane of glass measuring 2ft x 2 ft. In one hour 2.2 BTUs move across the glass. What is the R-value for this material? Show your work!
2. This apparatus is used again, but this time a 4.0 ft2 piece of 1” thick Styrofoam is used. Since it was lunch hour, the trial ran for two hours, during which .72 BTUs of energy moved across the Styrofoam. What is the R-value for 1” thick Styrofoam? Show your work!
3. Except for the small countries of Luxembourg, Bahrain, Qatar, and Oman, North America uses more energy per person than all other parts of the world. This is true because historically we have always had abundant energy in the form of wood, coal, and oil. Because we have had a large supply, there has been less interest in developing ways to use energy more efficiently. There are several categories of personal energy consumption that we all have some control over: heating and air conditions, heating water, lighting, transportation, and the purchase and use of efficient electrical appliances.
One of the major ways that energy leaves or enters buildings is through windows. A single-pane window has an R-value of 0.90.
a. An average house in the Valley has about 1,800 sq. feet of floor space, and 20 windows averaging 3.0 x 4.0 feet. If the average daytime outdoor temperature was 50.0 degrees F and the house thermostat was set at 70.0 degrees, how many BTUs would be lost through the windows during the 10.0 hours of daylight?
b. How many BTUs would be saved if the thermostat was set for 60 degrees?
c. In the summer season the average valley day-time temperature is 80 degrees. If the air conditioner were set for 65 degrees, how many BTUs would be drawn into the house (and need to be “removed”) in one 12 hour day?
d. ...in the 100 days that average this temperature?
e. Compare to a similar house with double pane glass (R-value of 1.85). How many BTUs would be saved (in the 100 days)by installing this glass in the house?
f. How many kWh of electricity (assuming 100% efficiency)
Energy Review Problems Worksheet
show all calculations with units
1/R = Energy (BTUs) Power(watts) = current(amps) x voltage(volts)
area (ft2)time (hr)∆T(°F)
BTU = energy needed to raise the temp. of 1 pound of water 1°F
1 gallon weights 8 pounds 1 cubic foot of gas contains 1031 BTUs
1 kWh = 3413 BTU 1 ton of coal contains 2.5 x 107 BTUs
1 MW (megawatt) = 1000 kW (kilowatts)
1. How many kWhs of energy could be generated by a coal burning power plant that burned 250 tons of coal and was 40% efficient?
2. How much natural gas must be burned in order to produce 52 MWhs of electricity if the power plant was 65% efficient?
3. How many pounds of water could raise in temperature 20°F by the 90% efficient burning of 30.0 cubic feet of natural gas?
4. a. The R-value of a hot water heater insulation blanket is 6.7 and covers an area of 25 square feet. How many BTUs will it save for every hour that it prevents 1°F of temperature change?__________
b. How many cubic feet of gas will that save in one year?
5. What is the efficiency of a gas-burning furnace that heats 5,000 lbs of water 25°F by burning 210 cubic feet of natural gas?
6. 7.0 tons of coal are burned to generate 3.6 x 104 kWh of electricity. What is the efficiency of the generator?
7. You replace one 75-watt incandescent light bulb with fluorescent light bulb that gives the same amount of light by drawing only 20 watts. You use the light bulb for an average of 4 hours a day.
a. How many kWhs of energy would you save in one day?
b. How many kWhs of energy would you save in one year?
c. The cost of one kWh is $0.10. How much money does the fluorescent light bulb save in one year?
8. a. How much power is produced by a solar cell that produces 0.06 amps of current and has a voltage of 0.75 volts?
b. if the solar cell had an area of 20 cm2 and collected sunlight when the solar constant (the amount of energy available per cubic centimeter) was 0.08 watts/cm2, what was the efficiency of the solar cell?
c. How many solar cells would it take to run a 60-watt bulb?
9. If the efficiency of a coal-burning power plant is 65% and the efficiency of energy transmission is 95%, and the efficiency of an electric stove is 85%, how many BTUs of heat could be produced by an electric stove after 0.50 tons of coal have been burned?
10. How many cubic feet of gas must be burned in a 80% efficient pool heater in order to increase the temperature of a 200,000 gallon pool from 60°F to 75°F?
Unit: Air Pollution and Climate Change
GET YOUR HOUSEHOLD GAS AND ELECTRIC BILL (THESE ARE TWO DIFFERENT BILLS)
Reading:
Chapter 15 Text
Section 15-1 through 15-7
Chapter 16 Text
Section 16-1 through 16-7
ONLINE READING QUIZ DUE DATE:__________
Labs:
Examining Evidence for Climate Change Lab
Ozone Lab (optional)
CO2 Lab
Worksheets:
Carbon Dioxide Diet Exercise
Kyoto Protocol Questions
Clean Air Act Worksheet
Global Warming and Sea Level Worksheet
Simple Math for Geniuses
Air Pollution and Climate Change Review Sheet
Global Warming
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Greenhouse Effect (how does it work)
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Greenhouse Gases (what are they, how are they produced)
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Types of Evidence
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Forcings and Feedbacks (solar output, albedo, volcanic ash, melting tundra, etc.)
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Possible Consequences
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Sources and Sinks for CO2
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Carbon Sequestration and Carbon Credits
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Relative Temperature Increases throughout History
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Thermohaline Circulation
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Possible Responses by Humans
Air Pollution
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Sources (Natural and Anthropogenic)
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Types of Pollutants (Primary and Secondary)
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NOx Reactions
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Factors Which Increase Air Pollution
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Thermal Inversions
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Photochemical vs. Gray (Industrial) Smog
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LA and Smog
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Acid Deposition (dry vs. wet)
Ozone and Ozone Depleting Compounds (ODC’s)
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Types and Locations of Ozone (what is its purpose)
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Natural Formation and Destruction of ozone
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Anthropogenic destruction of ozone
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CFC’s, halons, furans, and SF6, CCl4
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Effects of Thinning Ozone
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Details of Ozone “Hole” (characteristics, location, changes)
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Government Regulations of CFC’s (Montreal, London, Copenhagen)
Skin Cancer
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Keratoses
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Carcinomas
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Melanomas
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ABCD’s of Melanoma
Indoor Air Pollution
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Comparison with Outdoor Air Pollution
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Top Three Indoor Air Pollutants
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Where Indoor Air Pollutants can Lurk
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What to do about Indoor Air Pollution
Air Pollution Prevention
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Control vs. Prevention Solutions
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Industrial Control Options
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Catalytic Converters (and other options to reduce automobile emissions)
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Control of Acid Deposition
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Government Regulations of Pollution (Energy Policy Conservation Act, Clean Air Act, Kyoto Protocol)
Homework and Articles
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Lessons from CO2 Diet and Global Warming Problems
Measuring U.S. Climate Change
The two key factors in determining climate are temperature and precipitation. We will look at their fluctuations over the last century or so using the data on the website below. http://www.ncdc.noaa.gov/oa/climate/research/cag3/cag3.html
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Select the ‘Statewide’ Button. Realize that the data can also be analyzed on different scales (national, regional, etc.)
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Choose any state by clicking on it or the list at the bottom of the window.
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First select the ‘Mean Temperature’. Eventually we will also look at precipitation data for the same state and time period.
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Also be sure to select ‘Annual’ in the Period Menu.
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Leave all of the other settings as they are and click the ‘Submit’ button. It can take a while for the graph and information to load when many people are accessing the site simultaneously so be patient.
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When the information appears, record below the ‘Annual Trend’ for the time period shown. Remember, we want the Trend not the average temperature.
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Go back to the last page and select ‘Precipitation’. Then click on the ‘Submit’ button to display the precipitation information.
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When the information appears, record below the ‘Annual Trend’ for the period shown. Remember, we want the Trend not the average precipitation.
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Now repeat the above process for three more states. Choose states from a variety of areas/regions.
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State 1
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State 2
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State 3
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State 4
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Averages
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Temperature
Trend
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Precipitation Trend
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According to your results, what is happening to the climate (temp. and precip.) in the United States?
Is there a constant relationship between temperature change and precipitation change? If so, what is it? If not, why not?
Let’s change the scale at which we examine climate change in the U.S. Go back to the original page http://www.ncdc.noaa.gov/oa/climate/research/cag3/cag3.html and select the ‘National’ Button.
Now create a chart of the annual temperature and precipitation data for the entire U.S.
What do the data suggest about the climate trends for the entire country? Don’t forget to look at both temperature and precipitation data.
Does this analysis agree or disagree with the data you collected on a state level. Why or why not?
In the end, do the data prove, disprove, or support the assertion that global warming is occurring? EXPLAIN why or why not in specific detail?
Measuring and Interpreting
Tropospheric Ozone
Background:
There are two types of ozone (O3). Stratospheric ozone is found high up in earth’s atmosphere and does the vitally important job of absorbing ultraviolet (UV) radiation before it reaches earth’s surface. It’s the ‘good’ ozone. Without stratospheric ozone, biological molecules would be “cooked” by the penetrating UV radiation and living organisms would suffer as a result. This lab focuses on the other kind of ozone- tropospheric ozone.
Tropospheric ozone is a potential human health threat because of its highly reactive nature and ability to form other tertiary pollutants. This ground-level ozone or 'bad' ozone is formed when nitrogen oxides (NOx) and volatile organic compounds (VOC), collectively called 'ozone precursors', react with sunlight. Emissions from car exhausts, power plants and industrial facilities are the major sources of NOx and VOC. Another key component in ozone formation is the presence of sunlight. Given the right conditions, this tropospheric ozone can ultimately react to form photochemical smog- the brown air we’ve come to know in Los Angeles.
Procedure:
In this lab we will monitor tropospheric ozone concentrations over the period of several days to determine if any patterns develop. We will be using “badges” that change color when exposed to ozone and a device (called a Zikua ozone meter) that interprets that color change. Badges will be exposed to ambient air for periods of one hour after which they will be evaluated using the Zikua ozone meter. When one badge has been measured, another badge will be exposed to the ambient air for the next hour. This will continue throughout an 8 hour day for three days. We will also leave one badge exposed for all 8 hours of the day to determine the total daily exposure of ozone. All ozone levels will be recorded on an excel spreadsheet for later anaylsis.
Given the above information and your understanding of tropospheric ozone formation, create a hypothesis about ozone concentrations over the period of an 8 hour day. Assume that we have a typically sunny, clear, and warm spring day.
Hypothesis:
Once we have collected the ozone measurements for three days, you should be able to complete the following.
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Construct a graph that charts ozone levels for each 8 hour day. Put all three or four days on the same graph and label it accordingly (axes and legend). Each data point should be an average of the two readings taken at each time.
Plotting only the data points (an X-Y scatter) makes it difficult to interpret the daily trends. How could you illustrate or show the trends more clearly? DO SO on your graph either before or after you print the graph. Remember: Your graph should be constructed so that you can see how ozone levels changed over the period of a day and how each separate day compares to the others.
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Are there any patterns to ozone formation over the period of a day? If so, what are they?
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Is there any discrepancy between the data for the 3 different days? How well do the data from each day agree with the other days?
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Calculate the average hourly ozone concentration for the 3 days. That means, find the average 0800 reading, the 0900 reading, etc.. Plot these averages on a graph so you can see how the average ozone levels changed over time. Include a ‘best fit’ curve.
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Does this graph change your interpretation of ozone fluctuations over an 8 hour day? If so, why? If not, why not?
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Which graph is better at illustrating the fluctuations in ozone levels? Explain why you believe the graph to be ‘better’.
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How do the 8 hour total measurements help us understand ozone formation patterns?
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Compare our results to your original hypothesis. Does the data support your hypothesis? Explain.
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How do our result compare with the Air Quality Index Chart that your teacher gave you?
Note: Unhealthy levels are >150 and Very Unhealthy is >200
Check out this link for some helpful hints: http://airnow.gov/index.cfm?action=aqibroch.aqi#intro
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