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Ozone in the stratosphere

Journal Article · · Environ. Sci. Technol.; (United States)
OSTI ID:5745333
The chemistry of ozone in the atmosphere begins with absorption of solar ultraviolet radiation by O/sub 2/ molecules in the stratosphere. Chemical bond rupture occurs, and ozone is produced. If nitric oxide, NO, is somehow introduced into the stratosphere, a chain reaction takes place. The NO and NO/sub 2/ reactions furnish a true catalytic cycle in which NO and NO/sub 2/ are the catalysts. Because of these reactions, oxides of nitrogen directly introduced into the stratosphere are expected to destroy ozone. This was the basis of the first perceived threat of the ozone layer - larger fleets of supersonic aircraft depositing oxides of nitrogen via their engine exhausts. Nuclear explosions also produce copious quantities of oxides of nitrogen. In 1974, concern was raised about other man-made atmospheric pollutants, especially the chlorofluoromethanes. It was recognized that they could enter into their own catalytic cycle, destroying ozone in a manner exactly analogous to the destruction caused by the oxides of nitrogen. 3 figures.
OSTI ID:
5745333
Journal Information:
Environ. Sci. Technol.; (United States), Journal Name: Environ. Sci. Technol.; (United States) Vol. 20:4; ISSN ESTHA
Country of Publication:
United States
Language:
English