|Office of Air Quality
February 24, 1997
To help students understand ozone pollution and make them aware of how it is formed.
4th and 5th grades
Environmental Essential Elements Across the Curriculum - 75.25 (4th grade) (3) Classify, order, and sequence data. The student shall be given opportunities to (B) classify matter and energy, organisms, actions, and events from the environment according to similarities and differences. (4) Communicate data and information in appropriate oral and written form. The student shall be given opportunities to (D) describe changes that occur to objects and organisms in the environment.
75.25 (5th grade) (4) Communicate data and information in appropriate oral and in appropriate form. The student shall be given opportunities to: (B) describe objects, organisms, and events from the environment, (D) describe changes that occur to objects and organisms in the environment.
Student will simulate the development of smog and infer how it occurs in nature.
Hold up a news headline about air pollution. Ask if anyone knows what ozone pollution or smog is.
Ozone is the same molecule regardless of where it is found, but its significance varies. Stratospheric ozone is found 9 to 18 miles high where it shields us from harmful ultraviolet rays from the sun. High accumulations of ozone gas in the lower atmosphere at ground level is air pollution and can be harmful to people, animals, crops and other materials.
Elevated levels above the national standard may cause lung and respiratory disorders. Short-term exposure can result in shortness of breath, coughing, chest tightness, or irritation of nose and throat. Individuals exercising outdoors, children, the elderly, and people with pre-exiting respiratory illnesses are particularly susceptible. Chemists have found that the materials damaged by ozone include rubber, nylon, plastics, dyes, and paints.
Ozone pollution, a component of smog, is mainly a daytime problem during summer months because sunlight plays a primary role in its formation. Nitrogen oxides and hydrocarbons are known as the chief "precursors" of ozone. These compounds react in the presence of sunlight to produce ozone. The sources of these precursor pollutants include cars, trucks, power plants and factories, or wherever natural gas, gasoline, diesel fuel, kerosene and oil are combusted. These gaseous compounds mix like a thin soup in the atmosphere, and when they interact with sunlight, ozone is formed.
Large industrial areas and cities with heavy summer traffic are the main contributors to ozone formation. When temperatures are high and the mixing of air currents is limited, ozone can accumulate to unhealthful levels.
Weather conditions such as lack of wind or a "thermal inversion" can cause smog to build up in an area. A thermal inversion occurs when a layer of warm air settles over a layer of cool air that lies near the ground. This condition prevents the smog from rising and scattering. Mountain ranges near cities may also trap smog in an area.
This activity should be done with adult supervision. Do not breathe in the "smog."
See the Ozone "Information, Activities and Data" page for suggested activities using ozone data collected by the Texas Natural Resource Conservation Commission and provided in the Texas Cities Data, Houston and El Paso Data for 1993 and Houston Data for 20 Years files.
Does your local newspaper or weather channel have a pollution index or other type of report on pollution in your area? Record this information over several days and see how it changes.
Taken from: Dr. Milton Payne's Outdoor Education Class. Spring 1994. Dr. Milton Payne, Department of Elementary Education, Stephen F. Austin State University, P.O. Box 13017, Nacogdoches, TX 75962.
Lois Myers and Kelly West, Teaching Environmental Sciences Class, Stephen F. Austin State University, 1995
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