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Find more facts and information on our topic page about ozone

ozone layer

A Dictionary of Earth Sciences | 1999 | | © A Dictionary of Earth Sciences 1999, originally published by Oxford University Press 1999. (Hide copyright information) Copyright

ozone layer The atmospheric layer at 15–30 km altitude, in which ozone (O3) is concentrated at 1–10 parts per million. Ozone also occurs in very low concentration at altitudes of 10–15 km and 30–50 km. Generally, atmospheric ozone is produced by the photochemical dissociation of oxygen (O2), resulting from absorption of ultraviolet solar radiation, to form atoms of oxygen (O). These atoms collide with molecular oxygen (O2) to form ozone (O3), which in turn absorbs solar radiation for further dissociation to O and O2. The ozone layer limits the amount of ultraviolet radiation reaching the ground surface. See also ATMOSPHERIC STRUCTURE.

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AILSA ALLABY and MICHAEL ALLABY. "ozone layer." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. 1 Dec. 2009 <http://www.encyclopedia.com>.

AILSA ALLABY and MICHAEL ALLABY. "ozone layer." A Dictionary of Earth Sciences. 1999. Encyclopedia.com. (December 1, 2009). http://www.encyclopedia.com/doc/1O13-ozonelayer.html

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