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33 Cards in this Set
- Front
- Back
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Natural Chemical Cycles
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Nitrogen and Carbon cycles
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Naturally generated pollutants
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SO2, H2S from volcanoes, CO2 from forest fires, NO - NO2 - O3 from lightning
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At sea level dry air consists of the following percentages by volume of these molecules...
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N2 - 78%
O2 - 21% Ar - 1% CO2 - 0.03% And trace amounts of others |
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Levels of the Atmosphere in order from lowest to highest and their altitudes
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Troposphere - 0 to 10km
Stratosphere - 10 to 50km Mesosphere - 50 to 200km Thermosphere - above 200km |
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Chemical Processes by Atmospheric Region:
Troposphere |
Contains 80% of total mass and almost all of the water vapor (H20 g)
Temperature decreases |
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Chemical Processes by Atmospheric Region:
Stratosphere |
Consists of Nitrogen, Oxygen, and Ozone
Temperature increases due to exothermic reactions |
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Chemical Processes by Atmospheric Region:
Mesosphere |
Low concentrations of gases
Temperature decreases |
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Chemical Processes by Atmospheric Region:
Thermosphere |
Consists of N2, N, O2
Temperature increases due to bombardment of gas mocs by electrons and protons from the sun |
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Photoionization
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Absorbtion of dangerous photons:
Results in loss of an electron --> NO + hv --> NO+ + e- Occurs in the mesosphere and thermosphere |
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Photodissociation
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Absorbtion of dangerous photons:
Results in dissociation of moc --> O2 + hv --> O + O --> O2 Occurs in the mesosphere and thermosphere |
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Ozone
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Natural process:
O2 + uva 240nm --> O + O M + O + O2 --> O3 + M Principle absorber of UV radiation from 240 to 300 nm |
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Ozone Depletion
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Ozone is normally found in the stratosphere but that is where it is being depleted
Ozone reaction with CL atoms formed from UV dissociation of Freons results in: OZONE DEPLETION |
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Freons - Common Uses and why it was thought to be so great
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Chlorofluorocarbons used in AC, Spray propellants, Foam products
Non-toxic Non-reactive Non-flammable |
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Freons in the Stratosphere
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Ultraviolet radiation could break C-Cl bonds in freons:
CFCl3 + uv -->CFCl2 + Cl or CF2Cl2 + uv -->CF2Cl + CL |
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Freed Cl from Freons plus Ozone
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Cl acts as a catalyst for Ozone depletion:
Cl + O3 --> ClO (intermediary) + O2 ClO + O --> Cl + O2 = O3 + O --> 2 O2 Each Cl can destroy 10^4 to 10^5 O3 molecules |
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What else can destroy O3?
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High Altitude Aircraft and Some natural processes produce NO, NO2 which can destroy Ozone:
O3 --> O2 + O NO + O3 --> NO2 + O2 = 2 O3 --> 3 O2 |
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Montreal Protocol of 1987
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It was thought that Ozone depletion could have very negative side effects such as skin cancer
Most countries agreed to stop using Freons ( which was Epic) Believed Ozone problem would fix itself (that has been seen to be true) |
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Greenhouse Effect:
Solar Radiation |
In the visible region (400 - 700 nm) is being absorbed by the earth's surface
Earth then radiates energy in the infrared region: Mean temp of the earth is rising significantly |
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Greenhouse Effect:
Asymmetric Stretch |
Some mocs are capable of changing their dipole moments which allows them to absorb infrared light
Causes them to lose heat to the troposphere by collisions |
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Greenhouse Effect:
Greenhouse Gases - H2O |
H2O - Atmospheric concentration is constant (raises the temp of the earth and allows it to be habitable) Not a problem
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Greenhouse Effect:
Greenhouse Gases - CO2 |
CO2 levels have increased 25% over pre-industrial values
10^10 tons of CO2 generated per year by transportation, power production, industry, and home heating (adds 1 ppm annually to the atmosphere) |
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Greenhouse Effect:
Greenhouse Gases - Others |
CH4, NO2, Freons increase to human activity
Freons are very potent greenhouse gases |
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Greenhouse Effect:
Global Warming |
Causing weather patters to change
Volcanic eruptions and reduction of CFC's may somewhat offset CO2 affects but only viable solution is decrease of CO2 emissions |
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pH of regular rain
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about 5.5 - 5.6 because of normal CO2 concentrations in the atmosphere
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Acid Rain - the formation
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has a pH below 5.6
SO2 from metal extraction, burning of sulfur containing coal, NO2 and other acid anhydrides can lower pH to 4.3 Covalent oxides react w/ water to produce acids (acid anhydrides) |
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Acid Rain - the effects
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Toxic to aquatic life and vegetation
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Acid Rain - the solutions
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Develop practical and inexpensive ways to remove SO2 from effluent gases
Installation of H2SO4 manufacturing facilities near SO2 sources |
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Photochemical Smog:
Compounds involved |
Primary pollutants - NO, CO, Hydrocarbons (from vehicle exhaust)
result in formation of Secondary Pollutants - NO2, O3 ( these actually cause smog) |
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Photochemical Smog:
Ozone Reactions |
O3 reacts with C==C bonds in rubber, lung tissue, and other biological substances (gasoline)
O3 rxns produce mocs like PAN and various Organic intermediates which form aerosoles (liquid droplets) and scatter sunlight to form Haze |
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Photochemical Smog:
Sunlight |
Sunlight is important in the rxns
Cause peak concentrations of smog at certain times of the day |
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London Smog (Industrial Smog):
Components |
Burning coal produces SO2, Ash, Soot, and CO
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London Smog (Industrial Smog):
Effects |
SO2 forms H2SO4 which leads to (NH4)2SO4 aerosol which is damaging to lungs
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London Smog (Industrial Smog):
Events |
Dec 1952, 4000 to 8000 deaths caused by smog in London
1948, deaths in Donora, PA Lead to US Clean Air Act |