| Protecting the Earth |
| Monday, 28 April 2008 | |
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Discoverers
Leon TEISSENREC BORT of highlights in 1902 the role of the ozone layer that absorbs solar radiation (UV actually). In 1974 two American scientists: Mario Molina and F. SHERWOOD ROWLAND made for the first time the theory of depletion of the ozone layer under the impact of Chlorofluorocarbons (CFCs), appeared in 1938. And J. FARMAN British Antarctica Survey (BAS) announced in 1985 that a "hole" temporary but important (up 50% loss) appears each spring in the ozone layer over Antarctica since 1979 and resolves to early fall. Evolution of the hole in the ozone layer What is ozone? The ozone (O3) is a specific chemical form of oxygen, very unstable and reactive. Ozone is generated by including the bombing of the oxygen molecule stable O2 by utraviolets (UV). Condition critical: the presence of oxygen that was produced in large quantities with the proliferation of photosynthetic micro-organisms in the Precambrian. {mosgoogle center}The ozone layer is schematically part of the atmosphere where its concentration is highest. Thus, ozone is more present at a distance of ground between 15 and 40 km (more heavily toward 35 km) with a concentration around 8 ppmv, a layer called the stratosphere. Hence the appellation stratospheric ozone not to be confused with ground-level ozone induced largely by vehicular traffic and particularly irritates the eyes and respiratory tract. |
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| Last Updated ( Tuesday, 17 February 2009 ) |