Transcript Slide 1

Air Pollution: Chapter 12
What’s in the air?
O3, NO, NO2, CO, CO2, SO2, HCHO
And other things like particulates and Black Carbon!
Types and Sources of Pollutants
• primary and secondary pollutants
• Gases and particulate matter
• Gases: Carbon monoxide, Sulfur Dioxide,
Nitric Oxide, Nitrogen Dioxide
• Particulates are classified by size (PM10,
PM2.5—diameter size in microns 2.5 μm)
Pollutants can be classified as primary pollutants
and secondary pollutants.
Primary Pollutants
Carbon Monoxide (CO): is a tasteless, colorless
and odorless gas.
Sources of CO include: fossil-fuel combustion
(Incomplete combustion in autos, trucks and
airplanes, some industrial process), biomass
burning, and photolysis reactions.
Concentrations of CO in urban air are typically 2-10
ppmv. On freeways and in traffic tunnels values
rise to more than 100 ppmv.
Primary Pollutants
Sulfur Dioxide (SO2): is a colorless gas that
exhibits a taste at levels of 0.3 ppmv and a strong
odor at levels greater than 0.5 ppmv.
Sources of SO2 include: coal-fired power plants,
automobile tailpipes, and volcanoes.
Background concentrations in the troposphere
range from 10 pptv to 1 ppbv. In polluted air, 1-30
ppbv.
Primary Pollutants
Nitrogen oxides are gases that form when some of
the nitrogen in the air reacts with oxygen during the
high-temperature combustion of fuel.
Nitric Oxide (NO): is a colorless gas and a free radical.
Precursor to tropospheric ozone.
Sources include: fossil-fuel combustion/autos and
planes, and biomass burning.
Nitrogen Dioxide (NO2): is a brown gas with a strong
odor. Absorbs short wavelengths. Intermediary
between NO and O3 production.
Primary Pollutants
Background concentrations range from 20 to 50
pptv. In urban areas, concentrations are 0.1-0.25
ppmv. In midmorning NO2 is more prevalent than
during midday because sunlight breaks down most
NO2 past midmorning.
NOx = NO + NO2
Primary Pollutants
Volatile organic compounds (VOCs) represent a
class of organic compounds that are mostly
hydrocarbons-individual organic compounds
composed of hydrogen and carbon.
Methane (naturally occurring) is the most abundant.
Others include: benzene, formaldehyde (HCHO)
Secondary Pollutants
Secondary pollutants form chemically in the air. Ozone is a
secondary pollutant in the troposphere.
Ozone (O3): is a relatively colorless gas. Ozone exhibits an
odor at concentrations of 0.02 ppmv or greater. Ozone has a
sweet smell (Copy machine).
Ozone is not emitted. Background concentrations in
troposphere are 20 to 40 ppbv. In urban air, concentrations
range from 0.01 ppmv at night to 0.5 ppm during afternoons
in the most polluted cities. Typical mixing ratios are 80-100
ppb in urban air.
In 2008, EPA lowered the 8 hr primary standard from 84
ppbv to 75 ppbv.
Chemistry of Photochemical Smog
Photochemical smog involves reactions among NOx and
VOCs in the presence of sunlight.
On a typical day, ozone forms following emission of NO and
VOCs. In polluted air, ozone production occurs along the
following lines. Sunlight dissociates NO2 into NO and atomic
oxygen:
NO2 + solar radiation
NO + O
The atomic oxygen combines with molecular oxygen
(in presence of a third molecule, M) to form ozone, as
O + O2 + M
O3 + M
The ozone is then destroyed by combining with nitric oxide, thus
NO + O3
NO2 + O2
Chemistry of Photochemical Smog
NO + O3
NO2 + O2
If sunlight is present, the newly formed NO2 will break down
into NO and atomic oxygen. The atomic oxygen then
combines with molecular oxygen to form ozone again.
Large concentrations of O3 can form in polluted air only if
some of the NO reacts with other gases without removing
ozone in the process.
Chemistry of Photochemical Smog
EPA Standards
National Ambient Air Quality Standards
(NAAQS)
• 75 ppb O3 for an 8-hour averaging period
• 120 ppb O3 for a 1-hour averaging period
The number of unhealthy days during 2003
Fig. 12-11, p. 338
The days exceeding 1-hr standard in LA
Air Quality Index (AQI)
Particulate Matter
Particulate Matter (PM) represents a group of solid particles
and liquid droplets that are small enough to remain
suspended in the air.
Collectively known as aerosols, this grouping includes solid
particles that may irritate people but are usually not
poisonous.
These include: soot, dust, smoke, and pollen. Some more
dangerous substances include asbestos fibers and arsenic.
Particulates are classified by size (PM10, PM2.5—diameter
size in microns 2.5 μm)
Black Carbon
Black Carbon is a primary aerosol component of Diesel Particulate Matter,
a known toxin and regulated pollutant by several regulatory agencies,
including the California Air Resources Board (CARB).
Diesel Particulate Matter is known to cause adverse health effects in
people who are exposed, including premature hospitalization, asthma
attacks, bronchitis, other respiratory and cardiovascular symptoms, and
premature death.
Black Carbon is the second leading cause of Global Warming.
Black Carbon is emitted as a primary pollutant to the atmosphere through
a variety of incomplete combustion of sources and fuels; BC concentration
cannot be modeled or predicted, it must be measured.
Black Carbon is NOT adequately characterized through PM-2.5 mass only
measurements, chemical speciation is necessary. (Magee Scientific)
Black Carbon
Aerosol black carbon (“BC”) is a particulate pollutant species
emitted from the combustion of any carbonaceous fuel.
The name “Aethalometer” is derived from the classical Greek
verb ‘aethaloun’, (αεφαλουν) meaning ‘to blacken with soot’. It
is this optically-absorbing material that the ‘standard’
Aethalometer measures.
The only known source of aerosol black carbon in the
atmosphere is the combustion of carbonaceous fuels. There
are no known significant biological, geological or
meteorological sources.
Factors that Affect Air
Pollution
The Role of the Wind
Dilution, Turbulence, Mixing
• “Dilution is the solution to pollution” - in the 1950s this motto
led to the construction of tall smokestacks for large factories.
Pollution was released higher in the atmosphere where winds
were stronger. Air quality improved locally but suffered
downwind.
Atmospheric stability determines where pollutants get transported
The Role of Stability and Inversions
• temperature lapse rates
• inversions
• mixing depth
• The mixing layer can often be easily seen from an airplane.
The Role of Atmospheric Stability
The Role of Topography
• cold air drainage
• air blockage by mountain ranges
Severe Air Pollution Potential
•
•
•
•
sources
high pressure
inversions
stagnation
• Some locations, like Los Angeles and Mexico City,
have an unfortunate combination of surrounding
topography, frequent inversions, abundant emissions
and plentiful sunlight - perfect conditions for
photochemical smog.
A strong subsidence inversion along the coast of Californiav
A strong subsidence inversion along the coast of California
Summary of Chapter 12
• Primary and secondary pollutants
-gases and particulate matter
• Photochemical smog formation
• Controls on air pollution:
- wind, stability, topography