Title: Chapter 17 Air
1Chapter 17Air Air Pollution
- You are what you breathe!
2The Atmosphere
- To understand human impacts on our air, we must
first know a few basic facts about it. - The atmosphere is composed of four layers
3The innermost layer is...
- The TROPOSPHERE
- 17 km over sea level
- Known as the weather-breeder
4Composition of the Troposphere Where you are
right now.
- Nitrogen - 78 (by volume)
- Oxygen - 21
- What happens if O2 fluctuates?
- H2O (g), argon, trace gases
- Carbon Dioxide - ONLY 0.037!
- The earths atmosphere has evolved and changed
over its 4.6 billion year history - What may be some important times in evolution?
5Remember the biogeochemical cycles???
6Gaseous Biogeochemical CyclingIts not a
personal problem!
- The burning of fossil fuels adds carbon, nitrogen
oxides and sulfur oxides to the atmosphere. - Nitrogen fertilizers also add NOx and gaseous
ammonia to the atmosphere - Burning coal and oil releases sulfur dioxide,
which can be converted into sulfuric acid. - What problems can disruption of these cycles
cause?
7What do you think AIR POLLUTION means?
- The presence of one or more chemicals in the
atmosphere in sufficient quantities and duration
to cause harm to humans, other forms of life, and
materials.
8Can there be natural air pollution?
- Particulates from soil forest fires
- volcanoes release SOx
- COx NOx released by forest fires
- Pollen from plants
- CH3 H2S from organic decay
- Sea salt
9What is Air Pollution?
- Stationary Mobile Sources
- Primary Pollutants
- directly emitted into troposphere and directly
harmful - react with one another, air, or uV to form...
- Secondary Pollutants
- Cities usually have more air pollution than rural
areas - What are Ozone Action Days?
- Why are they always on hot, sunny summer days?
10Primary Pollutants
CO
CO2
Secondary Pollutants
SO2
NO
NO2
SO3
Most hydrocarbons
HNO3
H2SO4
Most suspended particles
H2O2
O3
PANs
Most
and
salts
Natural
Sources
Stationary
Mobile
Fig. 17.4, p. 422
11Upper LayersPlanes fly here.
- Stratosphere, Mesosphere, Thermosphere
- The second layer is the stratosphere, which
extends roughly 20-50km above the earth. - the rise in temperature at the tropopause limits
mixing between the layers - less water and a higher concentration of ozone
than the troposphere
12Stratospheric Ozone
- Ozone (O3) is produced when oxygen interacts with
UV radiation from the sun - In the stratosphere, the ozone layer blocks 95
of the UV rays - Ozone at ground level is a dangerous pollutant
- Why is it important that these UV rays be blocked?
1340
25
35
20
Stratosphere
30
25
Stratospheric ozone
15
Altitude (kilometers)
Altitude (miles)
20
10
15
10
5
Troposphere
5
0
0
0
5
10
15
20
Fig. 17.3, p. 419
Ozone concentration (ppm)
1440
Nitric oxide
Nitrogen dioxide
Ozone
30
20
Parts per million
10
0
6
7
8
9
10
11
12
1
2
3
4
5
6
7
8
A.M.
Noon
P.M.
Time
Fig. 17.6, p. 424
15More on Air Pollution
- Presence of chemicals in sufficient quantities
and duration to cause harm to humans, other
organisms or materials - Natural sources
- pollen, dust, forest fires, volcanoes, methane,
hydrogen sulfide - Where do most anthropogenic (human caused)
pollution comes from? - power plants, factories and automobiles
16Major Classes of Air Pollutants
- Oxides of nitrogen, carbon and sulfur
- Volatile Organic Compounds methane, propane,
CFCs - Suspended particulate matter
- Photochemical Oxidants - O3 H2O2
- Radioactive substances Rn-222
- Hazardous air pollutants - benzene
17Six Common Air Pollutants
18And the other toxic stuff?
What are VOCs?
19Want to know more?
20Whats being dumped in your air?
21- What characteristics does Chicago have that
increase or reduce air pollution? - Think in terms of climate, precipitation,
topography, industry, population size
22Brown Smog
- Primary Secondary Pollutants react with
sunlight to produce OZONE - Noxious brown haze
- Smoke Fog Smog
- Eye Lung irritant
- Photochemical Smog Ozone, PANs and VOCs
- This is why ozone is good up high, bad nearby
23How to make Brown Smog Induce an asthma attack
- N2 O2 high Ts ? NO (from coal power plants)
- NO O2 ? NO2 (in the troposphere -- brown gas)
- NO2 H2O(g) ? nitric acid
- NO2 uV? NO O
- O O2 ? ozone
- HCs O2 NO2 ? PANS they oxidize things
24Solar radiation
Ultraviolet radiation
NO Nitric oxide
NO O2 ? NO2
O2 Molecular oxygen
NO2 Nitrogen dioxide
H2O Water
NO2 uV? NO O
Hydrocarbons
NO2 H2O(g) ? nitric acid
HCs O2 NO2 ? PANS
O O2 ? ozone
PANs Peroxyacyl nitrates
O3 Ozone
HNO3 Nitric acid
Aldehydes (e.g., formaldehyde)
Photochemical smog
Fig. 17.5, p. 424
25Gray Smog
- Industrial Smog from burning oil coal
- Made of SO2 H2SO4 Soot aerosols
- Smokestacks control local pollution. HOW?
- What abiotic factors affect smog?
26How to turn a perfectly sky blue day gray
- C from Coal O2 ? CO2 CO
- S from Coal O2 ? SO2 (suffocating gas)
- SO2 O2 ? SO3 which then reacts with water vapor
to produce sulfuric acid - Sulfuric Acid ammonia ? salts
27Temperature Inversionshot air on top
- Warmer air is less dense than cooler air so
when warm air is on top of cool air, pollutants
cant disperse and are stuck. - This is called a temperature inversion
28- Subsidence Inversion - warm air moves in above
cool air - Radiation Inversion - ground cools at night sun
warms air above - Harmful if these last for more than a day or two.
- LA has thermal inversions about half the year
29Warmer air
Inversion layer
Cool layer
Mountain
Mountain
Valley
Mountains block out sun to reverse nightly
radiation Mountains block out sun to reverse
nightly radiation temperature inversions
Fig. 17.8a, p. 426
30Inversion layer
Mountain range
Subsidence thermal inversions where high pressure
air from coast creates descending warm air masses
Fig. 17.8b, p. 426
31Ultra Fine Particles
Fine Particles
Large Particles
Sea salt nuclei
Fly ash
Carbon black
Pollens
Paint pigments
Tobacco smoke
Cement dust
Milled flour
Combustion nuclei
Coal dust
Oil smoke
Metallurgical dust and fumes
Photochemical smog
Insecticide dusts
Fig. 17.7, p. 425
0.001
0.01
2.5
10.0
100.0
Average particle diameter (micrometers or microns)
32Atmospheric pressure (millibars)
0
200
400
600
800
1,000
120
75
110
65
Thermosphere
100
90
55
80
Heating via ozone
Mesosphere
45
70
60
Altitude (miles)
Altitude (kilometers)
35
50
Stratosphere
40
25
30
15
Ozone layer
20
Heating from the earth
Troposphere
10
5
Pressure 1,000 millibars at ground level
0
80
40
0
40
80
120
Fig. 17.2, p. 418
(Sea Level)
Temperature (C)
33ACID DEPOSITION
34Acid rain
- NORMAL RAINWATER IS ACIDIC!!! (oddly enough)
- Water carbon dioxide react to dorm carbonic
acid, so natural rainwater has a pH of 5.6 - Anything below that is considered acid deposition
(or acid rain)
35Acids
- Release hydrogen ions in solution
- pH less than 7
- pH is tenfold
- pH directly related to H ions
- Rain pH 5.6 due to CO2
- What are examples produced in environment?
36Acid Deposition
- What do smokestacks emit?
- What effect do tall smokestacks have on the
environment? - What secondary pollutants are produced from
emissions?
37Acid Deposition
- What do smokestacks emit? Smokestacks emit SO2
and NOx - What effect do tall smokestacks have on the
environment? Reduce local air pollution but
increase regional air pollution. Blame Canada! - What secondary pollutants are produced from
emissions? - Nitric Sulfuric acids salts
38Acid Deposition Acid Rain
Acid deposition
Wet deposition Rain, snow, fog
Dry deposition particles
Fig. 17.9, p. 428
39Acid Deposition in the US
Coal Burning Industrial Emissions
pH 2.3 on mountain tops!
Fig. 17.10, p. 428
40From western Europe
From Ohio Valley
From China
From Canada
Potential problem areas because of sensitive soils
No natural buffers
Potential problem areas because of air
pollution emissions leading to acid deposition
Current problem areas (including lakes and rivers)
Fig. 17.11, p. 429
41China
Iran
Pakistan
Saudi Arabia
India
Myanmar
Arabian Sea
Thailand
Bay of Bengal
Ethiopia
Indian Ocean
Equator
Winter monsoon blows out and Spring monsoons
blows back
Percentage of direct sunlight intercepted
Very heavy 3545
Heavy 2035
Medium 1020
Fig. 17.12a, p. 429
42Acid Deposition and Humans
- Toxic metal leaching into drinking water
- Decreased visibility from sulfate particles
- Damage to structures, especially containing
limestone
- Decreased productivity and profitability of
fisheries, forests, and farms
43Limestone statue of queen victoria
44(No Transcript)
45Acid Deposition and Aquatic Ecology
- Undesirable plankton and mosses
- Fish populations decrease
- Fish populations disappear
- Decay at bottom
- Mosses may dominate nearshore
46Acid Deposition and Aquatic Ecology
- Al leachate fish cant breathe
- Toxic, fatty soluble Hg magnified
- Acid shock from runoff
- Lose buffering ability
47Acid Deposition and Aquatic Systems
- Acid shock
- Biological
- magnification of mercury
Fig. 17.13, p. 430
48Acid Deposition on Plants Soil
- Harm to forests and crops begins at pH 5.1
- Damaged waxy surface
- Impaired germination
- Essential plant salts leach
- Al3 prevents uptake of nutrients and water
- Toxic heavy metals
- Acid loving mosses hold water, remove air, kill
fungi - Weaken trees
49- Fig. 17.14, p. 432
- See Connections p. 431
50Whats being done?
- NAPAP National Acid Precipitation Assessment
Program
- Bad News
- adverse impact on forest ecosystems and waiting
for effects on others - tenfold increase in acidity in first 36 cm of
soil - Nitrate concentrations in atmosphere have not
decreases - No decline in acidity in sensitive aquatic
systems
- Good news
- Reductions in SO2 and NOx emissions
- Declines in acidity in midwest and northeast
- Sulfate concentrations have dropped in lakes
- SO2 and NOx and particulate matter decreases may
increase health - SO2 reduction benefits exceed costs
51Whats can be done to reduce Acid Deposition?
- Energy Efficiency
- Reduce Coal Use
- Natural Gas
- Renewable resources
- Low sulfur coal
- Smokestacks with scrubbers
- Motor vehicle exhaust
- Taxes
- Cleanup Liming and phosphates
52Solutions Preventing and Reducing Air Pollution
- National Ambient Air Quality Standards (NAAQS)
- Primary and secondary standards
- Output control vs. input control