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Abstract Ozone in the stratosphere protects the earth by absorbing harmful ultraviolet radiation from the sun. However, when ozone occurs in the troposphere, i.e., the air that we breathe, it is harmful to health. In this project you can use data from EPA monitoring stations to analyze the weather/climate conditions that can lead to harmful ozone levels.Objective The goal of this project is to investigate ozone levels over time using archived data for the United States from the AIRNow website. Introduction Ozone (chemical formula: O3) occurs naturally in the upper atmosphere (stratosphere). It absorbs potentially harmful ultraviolet radiation from the sun that would otherwise reach the earth's surface. Ozone in the stratosphere thus serves a protective function for life on earth. In the lower atmosphere (troposphere) ozone is produced by chemical reactions from nitrogen oxides (NOx, chemical compounds with various ratios of nitrogen and oxygen) and volatile organic compounds (VOCs). A compound is said to be "volatile" if it evaporates readily at normal outside temperatures. Both heat and sunlight are also required for the chemical reactions that produce ozone. Nitrogen oxides are produced in exhaust from factories, power plants, cars, and trucks. Chemical solvents and gasoline vapors are major sources for volatile organic compounds in the atmosphere (AIRNow, 2007a). Ozone is a highly reactive form of oxygen. The oxygen that we use for respiration (chemical formula: O2) is less reactive. Ozone can more readily form compounds with an unpaired electron in the outermost shell. These compounds, called free radicals, can cause chain reactions that cause indiscriminate damage to molecules in cells. Virtually any large molecule in the cell—proteins, carbohydrates, lipids, and DNA—can be damaged by free radicals. Enzymes (catalase, superoxide dismutases, and glutathione peroxidases) and anti-oxidant molecules from the diet (e.g., vitamins C and E) act as free radical scavengers, and protect cells from damage caused by free radicals. Since ozone formation in the troposphere requires heat and sunlight, ozone levels are more likely to rise when the temperature is high. However, other conditions, such as an increase in the pollutants from which ozone is formed, can also lead to ozone elevation. In this project, you can use map data from the U.S. Environmental Protection Agency and other government agencies (AIRNow, 2007c) to track ozone levels in your area under different seasonal conditions to find out when ozone levels are most likely to be elevated. Terms, Concepts, and Questions to Start Background Research To do this project, you should do research that enables you to understand the following terms and concepts:
Questions
Bibliography The AIRNow website has a page with flash animations that discuss how ozone is formed, how ozone acts as a protectant high in the atmosphere but as a pollutant at ground level, and the sources and dangers of particle pollutants. http://www.airnow.gov/index.cfm?action=airnow.main
A map of the current Air Quality Index for the continental U.S. can be found at the following website along with links to state and local regions.
For information on the effects of ozone on people, animals, and plants, see:
For information on how atmoshperic ozone is monitored, see:
Materials and Equipment To do this experiment you will need the following materials and equipment:
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| Figure 1. Air Quality Maps Calendar link. |
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| Figure 2. An example of monthly thumbnails of ozone concentrations for San Francisco, CA. |
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| Figure 3. An example of 8-Hour Average Peak Concentration Map. |
Variations
Credits
Andrew Olson, Ph.D., Science Buddies
Michelle Maranowski, PhD, Science Buddies
Last edit date: 2011-01-06 13:00:00
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