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33 Cards in this Set

  • Front
  • Back
Natural Chemical Cycles
Nitrogen and Carbon cycles
Naturally generated pollutants
SO2, H2S from volcanoes, CO2 from forest fires, NO - NO2 - O3 from lightning
At sea level dry air consists of the following percentages by volume of these molecules...
N2 - 78%
O2 - 21%
Ar - 1%
CO2 - 0.03%
And trace amounts of others
Levels of the Atmosphere in order from lowest to highest and their altitudes
Troposphere - 0 to 10km
Stratosphere - 10 to 50km
Mesosphere - 50 to 200km
Thermosphere - above 200km
Chemical Processes by Atmospheric Region:

Troposphere
Contains 80% of total mass and almost all of the water vapor (H20 g)

Temperature decreases
Chemical Processes by Atmospheric Region:

Stratosphere
Consists of Nitrogen, Oxygen, and Ozone

Temperature increases due to exothermic reactions
Chemical Processes by Atmospheric Region:

Mesosphere
Low concentrations of gases

Temperature decreases
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
Photoionization
Absorbtion of dangerous photons:
Results in loss of an electron -->
NO + hv --> NO+ + e-

Occurs in the mesosphere and thermosphere
Photodissociation
Absorbtion of dangerous photons:
Results in dissociation of moc -->
O2 + hv --> O + O --> O2

Occurs in the mesosphere and thermosphere
Ozone
Natural process:
O2 + uva 240nm --> O + O
M + O + O2 --> O3 + M

Principle absorber of UV radiation from 240 to 300 nm
Ozone Depletion
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
Freons - Common Uses and why it was thought to be so great
Chlorofluorocarbons used in AC, Spray propellants, Foam products

Non-toxic
Non-reactive
Non-flammable
Freons in the Stratosphere
Ultraviolet radiation could break C-Cl bonds in freons:
CFCl3 + uv -->CFCl2 + Cl
or
CF2Cl2 + uv -->CF2Cl + CL
Freed Cl from Freons plus Ozone
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
What else can destroy O3?
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
Montreal Protocol of 1987
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)
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
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
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
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)
Greenhouse Effect:

Greenhouse Gases - Others
CH4, NO2, Freons increase to human activity

Freons are very potent greenhouse gases
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
pH of regular rain
about 5.5 - 5.6 because of normal CO2 concentrations in the atmosphere
Acid Rain - the formation
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)
Acid Rain - the effects
Toxic to aquatic life and vegetation
Acid Rain - the solutions
Develop practical and inexpensive ways to remove SO2 from effluent gases

Installation of H2SO4 manufacturing facilities near SO2 sources
Photochemical Smog:

Compounds involved
Primary pollutants - NO, CO, Hydrocarbons (from vehicle exhaust)
result in formation of
Secondary Pollutants - NO2, O3 ( these actually cause smog)
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
Photochemical Smog:

Sunlight
Sunlight is important in the rxns

Cause peak concentrations of smog at certain times of the day
London Smog (Industrial Smog):

Components
Burning coal produces SO2, Ash, Soot, and CO
London Smog (Industrial Smog):

Effects
SO2 forms H2SO4 which leads to (NH4)2SO4 aerosol which is damaging to lungs
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