5.6 Depletion of Stratospheric Ozone

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Presentation transcript:

5.6 Depletion of Stratospheric Ozone

the progression of the Ozone hole over the antarctic from 1970 to 1997.

CFC’s can (and in some cases used to) be found in: aerosol sprays cleaning fluids freezers air conditioners refrigerators industrial solvents dehumidifers foam insulation

HCFC's are found in: heat pumps central air conditioners

Polar stratospheric clouds PSCs are part of the reason why the ozone hole is greater in polar regions. You need a recipe for this to occur. Methane (CH4) from anaerobic digestion CFCs from our known sources Ozone from the breaking and bonding of oxygen. Nitrogen Dioxide (NO2) from emissions These react to create the inert substances of Hydrochloric Acid and Chlorine Nitrate

These inert substances remain trapped in the polar regions because of the atmospheric circulation patterns and rotation of the Earth. Over time, more and more of these substances collect.

During the winter months when the temperatures drop below -80 degrees celsius, ice clouds form. These clouds provide the surface for the slow reaction between HCl + ClONO2 This releases the relatively harmless Cl2 back into the atmosphere, while the Nitric Acid freezes to the cloud. When the sun comes back out, the Cl2 disassociates into 2 x Cl, attacking the O3

Some effects on plant and animal tissue as UV radiation increases decrease in agricultural yields and a decrease in overall forest productivity cellular/DNA damage to fish larvae, plankton and other organisms at the bottom of food webs thus affecting all higher trophic levels in the food web. Increase in the rate of skin cancer (a decrease in 1% in the ozone layer is predicted to increase skin cancers by 10%.) Increase in Xeroderma pigmentosum Increase in cataracts and changes in the retina, in mammals. Sheep and cattle in Argentina and Chile are already suffering from this effect. Suppresses and depresses the immune systems in mammals.

Brief history and status at this point in time: 1978- U.S. banned CFC's as propellants in aerosol products 1985 British Antarctic Expedition reports holes in the Ozone layer 1987- "Montreal Protocol on Substances that deplete the Ozone Layer" 1990 - London protocol - International conference to control these chemicals. Signed by U.S. and 22 other countries. Limited production and use of CFC's 50% reduction in CFC production worldwide by 2000 Now signed by over 90 nations Revised to require the virtual phaseout of CFC production by 1996

Alternatives and replacements for CFC’s with pros and cons. HCFCs (hydrochloroflurocarbons) Positive aspect -break down more quickly in the atmosphere posing less danger to the ozone layer Negative aspect -if overused they could cause damage to the ozone layer in the same way as CFC’s. Redesigned appliances could use more energy than the original models. HFCs (hydrofluorocarbons) Positive aspect-do not contain chlorine and are therefore safe for the ozone layer Negative aspect -safety questions such as flammability and toxicity still unclear Hydrocarbons (such as butane and propane) Positive aspect – they are relatively cheap and readily available Negative aspect -can be flammable and poisonous and some increase ground- level pollution Ammonia Positive aspect -a simple alternative for refrigerators Negative aspect -must be handled carefully Water (and Steam) Positive aspect -effective for some cleaning applications