Ozone Layer

Melissa CoughlinLawrence D . KornreichCIH Environmental Science05 June 2007Ozone LayerIntroductionWhat is OzoneThe chemical springula for ozone is O3 . The ticket of ozone constitutes three atoms of atomic number 8 . Ozone is an allotrope of type O and is less still than the diatomic species O2 . Ozone is highly reactive form of type O . Ozone in the top(prenominal) layer of the aureole protects the ultraviolet lightness rays from reaching the earth sign on along on the other(a) hand ozone in the lower layer of the earth muster causes respiratory problems in living organisms . most 90 appropriate of ozone is present in the stratosphere (15 to 50 km altitude . Ozone has twain vital functions First , it is responsible for filtering break through astronomical wavelength band of ultraviolet solar beam of light , ray which would be lethal to the creatures of the earth if it arrived , the earth surface in full intensity . Second , ozone warms the upper layer of the stratosphere which is an grueling part of the mechanics of the weather phenomena of the earth atmosphere . The fishing gear of ozone in the upper atmosphere was first recognized by Cornu in 1879 and Hartley in 1880Formation of ozone layerThe formation of ozone layer is photochemical instrument . The ultraviolet rays strike the oxygen scraps splitting the oxygen blood corpuscle into two independent unstable atoms of oxygen . These unstable oxygen atoms in search of stability combine with the unplowed oxygen molecules to form less stable ozone . Since ozone is less stable ultraviolet rays further split it yielding oxygen molecule and oxygen atom . This process forms a chain and gets recurrent once more and again . This is a never close process . Ozone is a trace gas in the atmosphere . Even in the stratosphere where it is most concentrated , it forms only a few separate ! per million of the local atmospheric compositionDisc overy of ozone holeThe polar ozone hole was observed in 1985 .

A team of scientists from the British Antarctic look inform a very big seasonal diminish in ozone values measured over their station at Halley Bay in Antarctica Every class in folk and October , ozone levels were falling significantly , by rough 25 percent but sometimes by as much as 60 percent . The decline probably started around 1976 . entropy showed no significant changes during 1957 and 1975 but on that point were apparent changes from 1977 to 1984 . When scientists reported the Antarctic Ozone hole and , more significantly , that the impact of ozone depletion would take on increased risk of cataract and shin cancer and of reduced dust immunity the public , oddly in the north , became worriedDepletion of ozone in the stratosphereThe debates point towards the oxides of north and water-vapor from the pulsate of high flying aircraft . This was followed by a widely print argument that inert atomic number 17 containing compounds readiness significantly deplete stratospheric ozone . By 1985 , the concerns about nitrogen oxides were generally laid to restThe Montreal Protocol to the 1985 Vienna Convention for the tribute of , sign(a) on September 16 , 1987 is one of...If you ask to get a full essay, order it on our website: BestEssayCheap.com

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