1.
·
Donora
·
High
pressure system leads to stagnant air, radiation
inversion in valley traps pollutants, which become deadly (pg. 346).
This combination of weather and topography is a common
theme in many air pollution problems.
·
Clean Air Act (1970):
·
Led to creation of U.S. EPA (clean water
and clean air)
·
Focused on just six “criteria”
pollutants
“Criteria” Pollutant |
Chemical Formula |
NAAQS Standard |
Ozone |
O3 |
0.075 ppm (8 h) |
Carbon monoxide |
CO |
9 ppm (8 h) |
Sulfur dioxide |
SO2 |
0.03 ppm (annual) |
Nitrogen dioxide |
NO2 |
0.053 ppm (annual) |
Lead |
Pb |
1.5 micro g/ cu. m (quarterly) |
Particulate matter |
PM10
and/or PM2.5 |
15 micro g/ cu. m (annual) |
·
Established National
Ambient Air Quality Standards (NAAQS) for the criteria pollutants.
·
Air Quality Index (Table 12.2)
·
Primary pollutants – directly emitted from a source,
e.g., carbon monoxide (from tail pipes).
·
Secondary pollutants – formed in the atmosphere by
chemical reactions involving primary pollutants, e.g., ozone (from nitrogen
dioxide, volatile hydrocarbons and sunlight).
2.
3.
Sources
·
Table 12.1; Figure 12.2
·
Volatile organic carbon (VOC)
4.
Trends: it's getting better (Fig. 12.10)
5.
Meteorological Factors Affecting Air
Pollution (pg. 340)
· Winds (Figure 12.13)
·
Inversions (Figure 12.14, 12.15, 12.16)
·
Topography (Figure 12.18)
6.
Acid Deposition (Fig. 12.21, 12.22, 12.23)
·
Sulfur dioxide (SO2) is oxidized to sulfuric
acid (H2SO4)
·
Nitrogen dioxide (NO2) is oxidized to nitric
acid (HNO3)
·
Both these acids return to earth as “dry deposition”
or as “wet deposition”, i.e., in rain and fog.
·
On the east coast, where coal burning power plants
generate both SO2 and NO2, sulfuric acid is often the
dominant acid (about 3:1).
·
On the west coast, where little coal burning occurs,
sulfuric acid and nitric acid occur in about equal concentrations (about 1:1).
7.
Stratospheric Ozone
·
Stratospheric ozone occurs naturally. It
protects us from UV radiation and is the
cause of the stratospheric inversion layer. It accounts for 90%
of all the ozone in the atmosphere, but is restricted to the
stratosphere.
·
Manmade chemicals, especially Freons (chloroflorocarbons, CFCs), slowly
migrate up into the stratosphere where they breakdown and generate catalysts
that promote the rapid destruction of ozone.
·
The Antarctic ozone hole, a localized phenomenon that
occurs only in the S. hemisphere Spring (starting in October) is the best
example of stratospheric ozone depletion. Global average ozone depletion is much harder to quantify.
·
NASA Total Ozone Mapping
Spectrometer (TOMS) page