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Hydrochlorofluorocarbons

The Future Of Hcfcs



CFCs and HCFCs have contributed to our quality of life, particularly as valuable components in refrigeration and computer technology. However, their impact on the atmosphere has prompted several countries to agree to stop producing them. The Montreal Protocol on Substances that Deplete the Ozone Layer was signed by 43 countries in 1987 to limit and eventually eliminate the production and use of CFCs. When additional evidence emerged that the ozone layer was being damaged more quickly than originally thought, more than 90 countries signed an amendment to the Montreal Protocol in 1990. In the year 2000, CFCs were banned from use, and guidelines included new phaseouts for HCFCs and HFCs by the year 2020 if possible, and no later than 2040.



Other research is increasing the need to develop acceptable alternatives to HCFCs. In laboratory tests, male rats exposed to 5,000 parts per million (ppm) of HCFCs over a two-year period (equivalent to what humans working occupationally with the compound might experience over 30-40 years) developed tumors in the pancreas and testes. The tumors were benign and did not result in death for the tested rats. Nevertheless, this research resulted in the recommended eight-hour occupational exposure levels to HCFCs for humans being reduced from 100 ppm to 10 ppm.

Two possible alternatives to HCFCs are already being used successfully. Refrigerators that use propane gas, ammonia, or water as coolants are being tested in research laboratories, and are using up to 10% less energy than typical models using CFCs as a coolant. Telephone companies are experimenting with crushed orange peels and other materials to clean computer circuit boards, as substitutes for another important use of CFCs and HCFCs. Certain microorganisms are also being tested that degrade HCFCs and HFCs, which could help in controlling emissions of these compounds during manufacturing processes involving their use.

Resources

Books

Duden, Jane. The Ozone Layer. New York: Crestwood House, 1990.

Fisher, David E. Fire and Ice. New York: HarperCollins, 1990.

Fisher, Marshall. The Ozone Layer. New York: Chelsea House Publishers, 1992.

Gay, Kathlyn. Air Pollution. New York: Franklin Watts, 1991.

Jahn, F., M. Cook, and M. Graham. Hydrocarbon Exploration and Production. Developments in Petroleum Science. Vol. 46. The Netherlands: Elsevier Science, 2000.

Periodicals

MacKenzie, Debora. "Cheaper Alternatives for CFCs." New Scientist (June 30, 1990): 39-40.

Wallington, Timothy J., et al. "The Environmental Impact of CFC Replacement-HFCs and HCFCs." Environmental Science & Technology 28 (1994): 320A-326A.


Sally Cole-Misch

KEY TERMS


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Chlorofluorocarbons (CFCs)

—Chemical compounds containing chlorine, fluorine and carbon. CFCs were a key component in the development of refrigeration, air conditioning, and foam products.

Greenhouse gases

—Gases that contribute to the warming of the earth's atmosphere. Examples include carbon dioxide, HCFCs, CFCs, and HFCs.

Hydrofluorocarbons (HFCs)

—Chemical compounds that contain hydrogen, fluorine, and carbon atoms.

Montreal Protocol on Substances that Deplete the Ozone Layer

—An agreement signed by 43 countries in 1987, and amended and signed by 90 nations in 1990, to eliminate the production and use of compounds that destroy the ozone layer.

Ozone

—A gas made up of three atoms of oxygen. Pale blue in color, it is a pollutant in the lower atmosphere, but essential for the survival of life on Earth's surface when found in the upper atmosphere because it blocks dangerous ultraviolet solar radiation.

Ozone layer

—A layer of ozone in the stratosphere that shields the surface of Earth from dangerous ultraviolet solar radiation.

Stratosphere

—A layer of the upper atmosphere above an altitude of 5–10.6 mi (8–17 km) and extending to about 31 mi (50 km), depending on season and latitude. Within the stratosphere, air temperature changes little with altitude, and there are few convective air currents.

Troposphere

—The layer of air up to 15 mi (24 km) above the surface of the earth, also known as the lower atmosphere.

Ultraviolet radiation

—Radiation similar to visible light but of shorter wavelength, and thus higher energy.

Additional topics

Science EncyclopediaScience & Philosophy: Hydrazones to IncompatibilityHydrochlorofluorocarbons - Why Hcfcs?, The Good News And The Bad News, The Future Of Hcfcs