Chloromonoxide www.assignmentpoint.com.

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Chloromonoxide www.assignmentpoint.com

Chloromonoxide Evidence for the destruction has been linked to the catalytically active Chloro monoxide ClO. & Ozone profiles as one goes South. It is interesting to note how little Chloro monoxide effects the amounts of Ozone. www.assignmentpoint.com

Relationship between ClO. & O3 Ozone Layer Ozone, ppm Chlorine monoxide ,ppb 2.5 1.0 Ozone (O3) Chlorine monoxide ClO. 0.5 63oS Latitude 73oS www.assignmentpoint.com

Thickness of Ozone Layer The thickness of the Ozone Layer is expressed in Dobson units (DU) and is equivalent to 0.001 mm thickness of pure O3 at the density it would possess at ground level (1 atm) Equator = 250 DU Temperate Latitudes = 350 DU Subpolar regions = 450DU www.assignmentpoint.com

Other Ozone Depleters But has the reduction and removal of CFC’s solved the problem of the Ozone Hole ? Or could there be other causes that are producing the Ozone Hole. ? Could our pollution arising from NO2 and CO2 contributing factors ? www.assignmentpoint.com

Interactive Catalytic Forms Destruction: Halide Radicals destroy Ozone. The majority of Chlorine does not exit as Cl. or ClO.. The two major nonradical inactive as catalysts species in the Stratosphere are: HCl Hydrogen chloride ClONO2 Chlorine nitrate gas www.assignmentpoint.com

Interactive Catalytic Forms Formation of nonradical chlorine species. ClO. + NO2. ClONO2 Cl. + CH4 HCl + CH3. But HCl react with Hydroxyl Radical HCl + OH. H2O + Cl. ( ClO. & Cl. Catalytically Active ) www.assignmentpoint.com

Origin of Ozone Hole The major destruction of the hole in the lower atmosphere occurs as a result of special winter weather conditions when the chlorine stored as the catalytically inactive forms (HCl & ClONO2 ) are converted to the catalytically active forms (ClO. & Cl.) (This occurs in Polar Stratospheric Clouds) www.assignmentpoint.com

Ice crystal formation Nitric acid in the atmosphere forms from the reaction between OH.& NO2. Catalytically inactive to active chlorine occurs on the surface of ice crystals formed from water and nitric acid in the lower stratosphere in winter when the temperature drops to  -80oC over the South Pole. www.assignmentpoint.com

Possible Role of CO2 “ CO2 acts as a blanket in the lower atmosphere,” says Salawitch. “ To balance the books the Stratosphere has to cool” Thus CO2 could be contributing to helping PSC formation due to reduced temperatures in the stratosphere. New Scientist, 1 May 1999 p28 www.assignmentpoint.com

Impenetrable Vortex formation The usual warming mechanism from of O + O2 O3 + Heat is absent due to total darkness and the stratosphere becomes very cold. As a result the air pressure drops ( PV=nRT ) and due to the rotation of the earth an impenetrable vortex forms with winds up to 300km/hr www.assignmentpoint.com

PSC’s Matter cannot readily enter this vortex and the air inside is isolated and remains cold for many months. ( Mid October) The crystals formed by the condensation of the gases within the vortex form Polar Stratospheric Clouds which consist of crystals of trihydrate of Nitric Acid. www.assignmentpoint.com

HCL attachment Gas phase HCl attaches to the ice particle HCl HCl HCl Crystal HCl of HNO3.3H2O Ice Particle formed at low Temperature (-80oC) HCl HCl www.assignmentpoint.com

Role of ClONO2 Ozone Layer (Radicals in PSC) ClONO2 Cl2 HCl HCl HCl Crystal HCl Accumulates in Winter of HNO3.3H2O HCl HCl ClONO2 collides with HCl to form Molecular Chlorine www.assignmentpoint.com

Formation of Cl. Radicals Ozone Layer (Radicals in PSC) Cl. Cl.. ClONO2 UV light Summer HCl Cl2 HCl HCl Crystal HCl of Accumulates in Winter HNO3.3H2O HCl HCl When the Light in Summer appears Cl2 is converted to Cl. www.assignmentpoint.com

Hole Closure ClONO2(g) also reacts with water H2O(s) + ClONO2(g) HOCl(g) +HNO3(s) HOCl + UV light OH. + Cl. It is only when the vortex has vanished does chlorine predominate in its inactive forms and the hole closes. www.assignmentpoint.com

Dimer ClOOCl ClO. also builds up in the dark and this dimerizes to for a relatively stable species. ClO. + ClO. ClOOCl When the Sun Appears ClOOCl 2 Cl. + 2O. Which contributes to Ozone destruction. www.assignmentpoint.com

Antarctic and Arctic Vortexes Ozone Layer (PSC’s) The Antarctic vortex is more intense than the Arctic which is more sensitive to temperature. The Arctic vortex is broken down more readily by rise of planetary waves created when air flows over mountains. Current research is using a U2 type aeroplanes to probe PSC’s www.assignmentpoint.com

Possible Link Ozone Layer “But PSC’s were here long before any one had the bright Idea of putting CFC’s into refrigerators. It’s our pollution that’s reacting with clouds and causing the problem. And our CO2 that will make the clouds more prevalent.” “Possible link : Greenhouse & Ozone Hole ?” www.assignmentpoint.com

Further Reading Ozone Layer “The Hole Story” by G.Walker New Scientist, p24 , March 2000 Websites www.nilu.no/projects/theseo2000/ www.ozone-sec.ch.cam.ac.uk SOLVE, http :/cloud1.arc.nasa.gov/solve/ www.assignmentpoint.com