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Published byAlberta Hope Simpson Modified over 6 years ago
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Stratospheric Ozone Depletion
Normal Ozone formation in the stratosphere: O2 + O O then O3 + UV O2 + O then repeated. Chloroflourocarbons (CFCs) NOUN Any of several volatile, inert, saturated compounds of carbon, fluorine, chlorine, and hydrogen: used as refrigerants, foam-blowing agents, solvents, and, formerly, as aerosol propellants until scientists became concerned about depletion of the atmospheric ozone layer.
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CCl3F + UV CCl2F + Cl then Cl + O3 ClO + O2
The chlorine atom in CFCs rob an Oxygen atom from ozone molecule. CCl3F + UV CCl2F + Cl then Cl + O3 ClO + O2 Forms over Antarctic, because of ice crystals in the atmosphere which promote Cl atoms robbing O atoms from Ozone. Worst in the Antarctic Spring (September) due to a build-up of ice during winter. Montreal Protocol (International Treaty) banned CFCs More UV hitting the Earth increases skin cancer, causes crop damage and reduces the productivity of the ocean’s plankton.
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Burning of coal (mostly power plants for electricity) releases SO2 (sulfur dioxide) and the burning of petroleum (from transportation) releases NO2(nitric oxide). These combine with water in the atmosphere to create acid rain. 2SO2 + O2 2SO3 then SO3 + H2O H2SO4 (sulfuric acid)—the biggest culprit of acid rain 3NO2 + H2O 2 HNO3 + NO (Nitric Acid) Acid Deposition
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Acid Rain clouds blow north to Canada which makes the Canadians angry
Acid Rain clouds blow north to Canada which makes the Canadians angry Eh. Acid rain dissolves marble and limestone which can eat away at tombstones, statues and buildings. Acid rain causes environmental problems by changing soil chemistry and elevating aluminum in the soil hindering water and nutrient uptake by plants. Lakes become more acidic which hurts the organisms in the lakes and crops are damaged. Prevention methods include electricity conservation (turning off lights, Energy Star appliances etc.) and alternative fuel/high mpg/electric cars and transportation.
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Tropospheric Ozone Formation
Tropospheric ozone formation begins with the burning of petroleum oil which releases NOx out of the exhaust pipe. Volatile organic carbons which come from cars, solvents, vegetation, scented products also contribute to the formation of ozone. Tropospheric Ozone Formation
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NO2 + sunlight --> NO + O
O + O2 --> O3 Then, it cycles back: NO + O3 --> NO2 + O2 VOCs can speed up the reaction. : NOx + VOCs + sunlight --> O3 Ozone is much worse in the summer due to sunlight driving the reaction.
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Breathing ozone can trigger a variety of health problems including chest pain, coughing, throat irritation, and congestion. It can worsen bronchitis, emphysema, and asthma. Ground level ozone also can reduce lung function and inflame the linings of the lungs. Repeated exposure may permanently scar lung tissue. Ozone interferes with the ability of sensitive plants to produce and store food and harms their appearance.
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