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Catalyst: Air Pollution

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1 Catalyst: Air Pollution
Read the Case Study on page 525 in your textbook What two types of air pollution are the worst in Beijing? What was China’s plan to reduce air pollution during the Olympic Games? What factors could lead to unhealthy summer air even if the pollution sources are removed? How many Americans die per year from pollution related problems?

2 A Brief History of Air Pollution
The atmosphere has long been a sink for waste disposal. Natural photochemical smog recognized in 1550 Acid rain first described in 17th century

3 A Brief History of Air Pollution
Two big events: Donora fog in 1948 London smog event in 1952 Both cause by pollutants being trapped by weather events. Both killed numerous people. Could happen again in cities like Beijing or Mexico City

4 Point source: emit pollutants from one or more controllable sites

5 Fugitive source: generate air pollutants from open areas exposed to wind processes

6 Mobile Source of Air Pollution
Mobile source of air pollutants move from place to place while emitting pollutants. Automobiles, trucks, buses, aircraft, ships, and trains.

7 General Effects of Air Pollution
Affects many aspects of our environment Visual qualities Vegetation Animals Soil Water quality Natural and artificial structures Human health

8 General Effects of Air Pollution
Significant factor in human death rate for many large cities Athens, Greece- # of deaths higher on bad air quality days Hungary- 1 in 17 deaths contributed to air pollution US- 300,000 deaths/year, health cost $50 billion China- health cost $50 - $100 billion

9 General Effects of Air Pollution
Affect human health in several ways Toxic poisoning, cancer, birth defects, eye irritation, and irritation of respiratory system. Increased susceptibility to viral infections, causing pneumonia and bronchitis. Increased susceptibility to heart disease. Aggravation of chronic diseases, such as asthma and emphysema.

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11 General Effects of Air Pollution
Many air pollutants have synergistic effects Do greater damage to the lungs than a combination of the two pollutants would be expected to do based on their separate effects.

12 Primary and Secondary Pollutants
Primary pollutants - emitted directly into the air Secondary pollutants - produced through reactions between primary pollutants and normal atmospheric compounds.

13 Primary and Secondary Pollutants
In addition to human sources, our atmosphere contains many pollutants of natural origin. Release of sulfur dioxide from volcanic eruptions. Release of hydrogen sulfide from geysers and hot springs and from biological decay in bogs and marshes. Release of ozone in the lower atmosphere as a result of unstable meteorological conditions. Emission of a variety of particles from wildfires and windstorms. Natural hydrocarbon seeps.

14 Criteria Pollutants There are six criteria pollutants Sulfur dioxide
Nitrogen oxides Carbon monoxide Ozone Particulates Lead

15 Sulfur Dioxide SO2 Colorless odorless gas
Once emitted can be converted to sulfateSO4 Removed from atmosphere by wet or dry deposition Major human sources; coal power plants, industrial processes

16 Sulfur Dioxide Adverse effects depend on dose and concentration present Injury or death to animals and plants Corrosion of paint and metals Important precursor to acid rain

17 Nitrogen Oxides Occur in many forms in the atmosphere but largely emitted in two forms: Nitric oxide- NO Nitrogen dioxide- NO2 A yellow-brown to reddish-brown gas May be converted to NO32- Both subject to emissions regulation and contribute to smog NO2 major contributor to acid rain

18 Nitrogen Oxides Nearly all NO2 emitted from human sources
Automobiles and power plants that burn fossil fuels Environmental effects Irritate eyes and mucous membranes Suppress plant growth However when convert to nitrate may promote plant growth

19 Carbon Monoxide CO is a colorless, odorless gas
Even at low concentrations is extremely toxic to humans Binds to hemoglobin in blood. 90% of CO in atmosphere comes from natural sources 10% comes from fires, cars, and incomplete burning of organic compounds

20 Ozone and Other Photochemical Oxidants
Photochemical oxidants result from atmospheric interactions of nitrogen dioxide and sunlight. Most common is ozone- O3 Colorless gas w/ slightly sweet odor Very active chemically, oxidizes or burns Beneficial in the upper atmosphere

21 Ozone and Other Photochemical Oxidants
Because ozone is a secondary pollutant it is difficult to regulate. Health standards often exceeded in urban areas Effects include Kills leaf tissue at high concentration Damage eyes and respiratory system Even young, healthy people may have breathing difficulty on polluted days

22 Particulate Matter PM10 is made up of particles less than 10μm in diameter Present everywhere but high concentrations and/or specific types dangerous Much particulate matter easily visible as smoke, soot, or dust Includes airborne asbestos and heavy metals

23 Particulate Matter Of particular concern are very fine pollutants
PM 2.5- less than 2.5 μm in diameter Easily inhaled into the lungs, then absorbed into the bloodstream Ultrafine particles- <0.18 μm released by automobiles. Related to heart disease

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25 Particulate Matter When measured often referred to as total suspended particles (TSPs) Tend to be highest in large cities in developing countries

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27 Particulate Matter Recent studies estimate that 2 to 9% of human mortality in cites is associated w/ PM Linked to both lung cancer and bronchitis Especially hazardous to elderly and those w/ asthma Dust can be deposited on plants Interferes w/ absorption of CO2 and O2 and transpiration

28 Particulate Matter Block sunlight and may cause climate change.
Global dimming Gradual reduction in the solar energy that reaches the surface of Earth Cools the atmosphere Lessens global warming

29 Lead Lead is constituent of auto batteries and used to be added to gasoline. Lead in gas emitted into air w/ exhaust Spread widely around world in soils and water along roadways Once in soil can enter the food chain Lead now removed from gas in US, CAN, EU 98% reduction in emissions since 1970s

30 Air Toxics Among pollutants that are known or suspected to cause cancer or other serious health problems. Associated w/ long-term and short-term exposures Gases, metals, and organic chemicals that are emitted in relatively small volumes Cause respiratory, neurological, reproductive, or immune diseases

31 Air Toxics Standards have been set for more than 150 air toxics
E.g. hydrogen sulfide, hydrogen fluoride, chlorine gases, benzene, methanol, ammonia EPA estimates that the average risk for cancer from exposure to air toxics is about 1 in 21,000

32 Hydrogen sulfide Highly toxic corrosive gas easily identified by its rotten egg odor. Produced from Natural sources such as geysers, swamps, and bogs Human sources such as industrial plants that produce petroleum or that smelt metals. Effects of hydrogen sulfide include Functional damage to plants Health problems ranging from toxicity to death for humans and other animals.

33 Hydrogen Fluoride Extremely toxic gaseous pollutant
Released by some industrial activities Such as production of aluminum, coal gasification, and burning of coal in power plants. Even a small concentration (as low as 1 ppb) of HF may cause problems for plants and animals. Potentially dangerous to grazing animals because forage plants can become toxic when exposed to this gas.

34 Methyl Isocyanate An ingredient of a common pesticide Colorless gas
known in the United States as Sevin. Colorless gas Causes severe irritation (burns on contact) to eyes, nose, throat, and lungs. Breathing the gas in concentrations of only a few ppm causes violent coughing, swelling of the lungs, bleeding, and death. Less exposure can cause a variety of problems, including loss of sight.

35 Volatile Organic Compounds
Variety of organic compounds used as solvents in industrial processes Dry cleaning, degreasing, and graphic arts. Hydrocarbons Comprise one group of VOCs. Thousands of hydrocarbon compounds exist, including natural gas, or methane (CH4); butane (C4H10); and propane (C3H8).

36 Volatile Organic Compounds
Some VOCs react w/ sunlight to produce photochemical smog Globally 15% of hydrocarbons emissions are anthropogenic In the US 50% Primary human source automobiles

37 Benzene Additive in gasoline and an important industrial solvent.
Produced when gasoline and coal undergo incomplete combustion. Also component of cigarette smoke Major environmental source on and off road vehicles

38 Arcolein A volatile hydrocarbon that is extremely irritating to nose, eyes, and respiratory system. Produced from Manufacturing processes that involve combustion of petroleum fuels Component of cigarette smoke

39 Variability of Air Pollution
Problems vary in different regions of the country and the world. LA pollution mainly from mobile sources Ohio and Great Lakes point sources Also varies w/ time of year Smog a problem in summer when there is lots of sunshine Particulates a problem in dry months

40 Las Vegas: Particulates
Particulates a problem in arid regions Where little vegetation is present and wind can easily pick up and transport fine dust. Brown haze over Las Vegas partly due to naturally occurring PM 10 60% of the dust comes from new construction sites, dirt roads, and vacant land.

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42 Haze From Afar Air quality concerns are not restricted to urban areas.
North slope of AK has an air pollution problem that originates from sources in EE and Eurasia. Transported by the jet stream. Significant as we try to understand global air pollution.

43 Urban Air Pollution Whether air pollution develops depends on topography and meteorological conditions Determine the rate at which pollutants are transported away and converted to harmless compounds.

44 Influences of Meteorology and Topography
Meteorological conditions determine whether air pollution is a nuisance or major health problem. Primary adverse effect Damage to green plants and aggravation of chronic disease Usually low-level over long period of time However major disaster have occurred

45 Influences of Meteorology and Topography
In the lower atmosphere, restricted circulation associated w/ inversion layers may lead to pollution events. Atmospheric inversion- Occurs when warmer air is found above cooler air

46 Occurs primarily in summer and fall.
Occurs when cloud cover associated w/ stagnant air

47 Influences of Meteorology and Topography
Cities situated in a valley or topographic bowl are more susceptible to smog problems than cities in open plains. Surrounding mountains and inversions prevent pollutants from being transported by wind or weather systems. E.g. Los Angeles

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49 Potential for Urban Air Pollution
Determined by the following factors: 1. The rate of emission of pollutants per unit area. 2. The downwind distance that a mass of air moves through an urban area. 3. The average speed of the wind. 4. The elevation to which potential pollutants can be thoroughly mixed by naturally moving air in the lower atmosphere.

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51 Potential for Urban Air Pollution
Concentration of pollutants in the air is directly proportional to the first two factors. As either emission rate or down wind travel distance increase, so will the concentration of pollutants City air pollution decreases w/ increases in third and forth factors. The stronger the wind and the higher the mixing layer, the lower the pollution.

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53 Smog Term first used in 1905 as mixture of smoke and fog that produced unhealthy air. Two major types Photochemical smog (LA type smog or brown air) Sulfurous smog (London type smog, gray air, or industrial smog)

54 Smog Photochemical smog reaction involves sunlight, nitric oxides and VOCs Directly related to automobile use Sulfurous smog is produced by the burning of coal or oil at large power plants.

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58 Future Trends for Urban Areas
The optimistic view Air quality will continue to improve Because we know so much about the sources of air pollution and have developed effective ways to reduce it. The pessimistic view In spite of this knowledge, population pressures and economics will dictate what happens in many parts of the world, The result will be poorer air quality in many locations.

59 Future Trends for Urban Areas; The United States
LA is a good area to look at for strategies for pollution abatement. Air quality plan involving the entire urban region includes the following features: Strategies to discourage automobile use and reduce the number of cars. Stricter emission controls for automobiles. A requirement for a certain number of zero-pollutant automobiles (electric cars) and hybrid cars with fuel cell and gasoline engines.

60 Future Trends for Urban Areas; The United States
A requirement for more gasoline to be reformulated to burn cleaner. Improvements in public transportation and incentives for people to use it. Mandatory carpooling. Increased controls on industrial and household activities known to contribute to air pollution.

61 Future Trends for Urban Areas; The United States
Have focused on LA because the air quality is so poor for a significant portion of the year. However, many large and not so large US cities have poor air quality 30 days per year of unhealthy air resulting from ozone pollution.

62 Future Trends for Urban Areas; Developing Countries
Less developed countries w/ growing populations are susceptible to air pollution Don’t have the financial base necessary to fight air pollution E.g. Mexico City 25 million people 50,000 buses, millions of cars, LPG leaks In a natural basin w/ mountains surrounding it Perfect situation for severe air pollution problem

63 Future Trends for Urban Areas; Developing Countries
Attempts to reduce air pollution Shutting down oil refinery Ordering industrial plants to relocate Air pollution however will continue to be a problem if unable to control vehicle use and LPG leaks.

64 Pollution Control The most reasonable strategies for control have been to reduce, collect, capture, or retain the pollutants before they enter the atmosphere. Reduction of emissions through energy efficiency and conservation measures is preferred.

65 Pollution Control: Particulates
Particulates emitted from fugitive, point or area stationary sources are much easier to control. Point and area sources can be controlled by Settling chambers or collectors which cause particulates to settle out Fugitive sources Protecting open areas, controlling dust, reducing effects of wind

66 Pollution Control: Automobiles
Control of pollutants such as carbon monoxide, nitrogen oxides, and hydrocarbons is best achieved through pollution control for automobiles. Nitrogen oxides controlled by recirculating exhaust gas CO and hydrocarbons reduced by catalytic converter

67 Pollution Control: Automobiles
Automobile emission regulations plan in US has not been effective Pollutants may be low when car is new But many people do not maintain them properly Suggested that effluent fees replace emission controls Other strategies reduce the number or type of cars

68 Pollution Control: Sulfur Dioxide
Can be reduced through abatement measures performed before, during, or after combustion. Cleaner coal technology available but makes fuel more expensive. Switch to low-sulfur coal But transportation is an issue

69 Pollution Control: Sulfur Dioxide
Washing it to remove sulfur Iron sulfide settles out Ineffective for removing organic sulfur Coal gasification Converts coal to gas in order to remove sulfur Gas obtained is clean

70 Pollution Control: Sulfur Dioxide
Emissions from power plants can be reduced by removing the oxides from the gases in the stack Scrubbing (flue gas desulfurization) Occurs after coal is burned Gases treated w/ a slurry of lime or limestone Reacts to form calcium sulfite Can then be process into building materials

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72 Clean Air Act Amendments of 1990
Comprehensive regulations enacted by the U.S. Congress that address acid rain, toxic emissions, ozone depletion, and automobile exhaust. Buying and selling of sulfur dioxide emissions One step back occurred in 2003 when the president and EPA allowed companies to upgrade w/o new pollution controls.

73 Clean Air Act Amendments of 1990
Also calls for control of Nitrogen dioxides Reduced by 10 million tons Toxins Especially those causing cancer Ozone depletion in the stratosphere End production of all CFCs

74 Ambient Air Quality Standards
Important because they are tied to emission standards that attempt to control air pollution. Tougher standards set for ozone and PM 2.5 When challenged in court justices help that the EPA’s responsibility is to consider benefits to health not financial costs.

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76 Air Quality Index AQI is used to describe air pollution on a given day. AQI is determined from measurements of the concentration of five major pollutants: Particulate matter, sulfur dioxide, carbon monoxide, ozone, and nitrogen dioxide.

77 Air Quality Index An AQI value of greater than 100 is unhealthy.
Air pollution alert is issued if the AQI exceeds 200. Air pollution warning is issued if the AQI exceeds 300, hazardous to all people. If the AQI exceeds 400, an air pollution emergency is declared, and people are requested to remain indoors and minimize physical exertion.

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79 Cost of Air Pollution Control
Cost for incremental control in fossil fuel-burning may be a few hundred dollars per additional ton of particulates removed. For aluminum plant, may be several thousand per ton. Also, a point is reached at which the cost of incremental control is very high in relation to additions benefits.

80 Cost of Air Pollution Control
Economic analysis of air pollution includes many variables, some of which are hard to quantify. We do know the following: W/ increasing air pollution controls, the capital cost for technology to control air pollution increases. As the controls for air pollution increase, the loss from pollution damages decreases. The total cost of air pollution is the cost of pollution control plus the environmental damages of the pollution.

81 Ozone Depletion Ozone (O3)
Triatomic form of oxygen in which three atoms of oxygen are bonded. Strong oxidant and chemically reacts with many materials in the atmosphere. In the lower atmosphere, ozone is a pollutant. Highest concentration of ozone in the stratosphere

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83 Ultraviolet Radiation and Ozone
Ozone layer in the stratosphere called the ozone shield Absorbs most of the potentially hazardous ultraviolet radiation from the sun. Ultraviolet radiation consists of wavelengths between 0.1 and 0.4 μm Ultraviolet A (UVA) Ultraviolet B (UVB) Ultraviolet C (UVC).

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85 Ultraviolet Radiation and Ozone
Ultraviolet C (UVC) Shortest wavelength and most energetic of the types of ultraviolet radiation. Sufficient energy to break down diatomic oxygen (O2) into two oxygen atoms. Each of these oxygen atoms may combine with an O2 molecule to create ozone. UVC strongly absorbed in the stratosphere, and negligible amounts reach the Earth’s surface.

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87 Ultraviolet Radiation and Ozone
Ultraviolet A (UVA) Longest wavelength Least energy of the three types of ultraviolet radiation. UVA can cause some damage to living cells Not affected by stratospheric ozone, and is transmitted to the Earth’s surface

88 Ultraviolet Radiation and Ozone
Ultraviolet B (UVB) Energetic and strongly absorbed by stratospheric ozone Ozone is the only known gas that absorbs UVB. Depletion of ozone in the stratosphere results in an increase in the UVB that reaches the surface of the Earth.

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90 Ultraviolet Radiation and Ozone
Approximately 99% of all ultraviolet solar radiation (all UVC and most UVB) is absorbed by the ozone layer. Natural service function Protects us from the potentially harmful effects of ultraviolet radiation.

91 Measurement of Stratospheric Ozone
First measured in 1920s using Dobson ultraviolet spectrometer. Dobson unit (DU)- 1DU = 1 ppb O3 Now have measurements from all over the world for 30 years Ground based measurements first identified ozone depletion over the Antarctic. Concentrations have been decreasing since the mid-1970s “Ozone hole”

92 Ozone Depletion and CFCs
Hypothesis that ozone in the stratosphere is being depleted by CFCs First suggested in 1974 by Molina and Rowland. Based on physical and chemical properties of CFCs and knowledge about atmospheric conditions. Vigorously debated by scientists, companies producing CFCs, and other interested parties.

93 Ozone Depletion and CFCs
The major features of the hypothesis: CFCs emitted in the lower atmosphere are extremely stable. Unreactive in the and therefore have a very long residence time (about 100 years). CFCs eventually wander upward and enter the stratosphere. Once above the stratospheric ozone, they may be destroyed by UV radiation, releasing chlorine, a highly reactive atom.

94 Ozone Depletion and CFCs
The chlorine released then depletes the ozone. Depletion increases the amount of UVB radiation that reaches Earth’s surface. UVB is a cause of human skin cancers and is also thought to be harmful to the human immune system.

95 Emissions and Uses of Ozone Depleting Chemicals
CFCs have been used As aerosol propellants in spray cans Working gas in refrigeration and AC Production of Styrofoam No longer used in spray cans but use has increased in refrigerants.

96 Simplified Stratospheric Chlorine Chemistry
CFCs are transparent to sunlight, essentially insoluble Non-reactive in the oxygen-rich lower atmosphere When CFCs reach the stratosphere, reactions do occur. UVC splits up the CFC releasing chlorine, the following two reactions can take place: Cl + O3 → ClO + O2 ClO + O → Cl + O2

97 Simplified Stratospheric Chlorine Chemistry
This series of reactions is what is known as a catalytic chain reaction. Chlorine is not removed Reappears in the second reaction Repeated over and over Process considerably more complex Chain can be interrupted and Cl stored in other reactions

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99 The Antarctic Ozone Hole
Since 1958 ozone depletion has been observed in the Antarctic every Oct. Thickness decreasing and geographic area increasing

100 Polar Stratospheric Clouds
Form during the polar winter (polar night) Antarctic air mass isolated from the rest of the atmosphere Air circulates about the pole in Antarctic polar vortex. Forms as the isolated air mass cools, condenses, and descends.

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102 Polar Stratospheric Clouds
Type I polar stratospheric clouds When air mass reach a temp between 195 K and 190 K, small sulfuric acid particles are frozen and serve as seed particles for nitric acid (HNO3). Type II polar stratospheric clouds If temperatures drop below 190 K water vapor condenses around Type I cloud particles

103 Polar Stratospheric Clouds
During the formation nearly all the nitrogen oxides held in clouds Facilitates ozone depleting reactions When spring comes and sun returns it breaks apart Cl2 Chlorine can not be sequestered to form chlorine nitrate, one of its carbon sinks.

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106 An Arctic Ozone Hole? Polar vortex also forms over the North Pole
Weaker and does not last as long as Antarctic Ozone depletion does occur at the NP Major concern is ozone-deficient air moving southward over population centers.

107 Tropical and Midlatitude Ozone Depletion
Evidence suggests an increase in ozone depletion at midlatitudes over areas including the US and Europe. We know the most about ozone depletion in polar regions (particularly Antarctica), but depletion of ozone is a global concern.

108 The Future of Ozone Depletion
If the manufacture, use, and emission of all ozone-depleting chemicals were to stop today, the problem would not go away, millions of metric tons of those chemicals are now in the lower atmosphere, working their way up to the stratosphere. Several CFCs have atmospheric lifetimes of 75 to 140 years.

109 Environmental Effects
Several serious potential environmental effects Damage to food chain on land and in oceans (loss of primary production ) Damage to human health (skin cancers, cataracts, and suppression of immune system) UV Index measure of UV radiation on a given day

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111 Environmental Effects
Reduce the risk of skin cancer and other skin damage from UV exposure by: Limit exposure to the sun between the hours of 10 A.M.and 4 P.M. When possible, remain in the shade. Use a sunscreen with an SPF of at least 30. Wear a wide-brimmed hat and, where possible, tightly woven full-length clothing. Wear UV-protective sunglasses. Avoid tanning salons and sunlamps. Consult the UV Index before going out

112 Management Issues The Montreal Protocol
Outlined a plan for the eventual reduction of global emissions of CFCs to 50% of 1986 emissions Elimination of the production of CFCs by 1999 Assessment of the protocol suggest that CFCs will return to pre-1980 levels by 2050

113 Management Issues Substitutes for CFCs hydrofluorocarbons (HFCs) and
Do not contain chlorine. However, fluorine atoms participate in reactions similar to those of chlorine but approximately 1,000 times less efficient in those reactions hydrochlorofluorocarbons (HCFCs). Contain an atom of hydrogen in place of a chlorine atom. Can be broken down in the lower atmosphere. However, cause ozone depletion if they do reach the stratosphere before being broken down.

114 Management Issues Short-term Adaptation to Ozone Depletion
Given the nature of problem and the atmospheric lifetimes of the chemicals that produce the depletion people will be learning to live with higher levels of exposure to ultraviolet radiation. In the long term, achievement of sustainability w/ respect to stratospheric ozone will require management of human-produced ozone-depleting chemicals.


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