1. Chapter 20 Air Pollution

2. Overview of Chapter 20  Atmosphere as a Resource  Types and Sources of Air Pollution  Effects of Air Pollution  Controlling Air Pollution in the US  Ozone Depletion in the Stratosphere  Acid Deposition  Air Pollution Around the World  Indoor Air Pollution

3. Atmosphere as a Resource  Atmospheric Composition  Nitrogen: 78.08%  Oxygen: 20.95%  Argon: 0.93%  Carbon dioxide: 0.04%  Ecosystem services  Blocks UV radiation  Moderates the climate  Redistributes water in the hydrologic cycle

4. Air Pollution - Terminology  Air Pollution  Chemicals added to the atmosphere by natural events or human activities in high enough concentrations to be harmful  Two categories  Primary Air Pollutant  Harmful substance that is emitted directly into the atmosphere  Secondary Air Pollutant  Harmful substance formed in the atmosphere when a primary air pollutant reacts with substances normally found in the atmosphere or with other air pollutants, or with sunlight

5. Major Air Pollutants

7. Major Classes of Air Pollutants  Particulate Material  Nitrogen Oxides  Sulfur Oxides  Carbon Oxides  Hydrocarbons  Ozone

8. Particulate Material  Thousands of different solid or liquid particles suspended in air  Includes: soil particles, soot, lead, asbestos, sea salt, and sulfuric acid droplets  Dangerous  May contain materials with toxic/carcinogenic effects  Small particles can become lodged in lungs

9. Nitrogen and Sulfur Oxides  Nitrogen Oxides  Gases produced by the chemical interactions between atmospheric nitrogen and oxygen at high temperature  Greenhouse gases that cause difficulty breathing  Sulfur Oxides  Gases produced by the chemical interactions between sulfur and oxygen  Causes acid precipitation

10. Carbon Oxides and Hydrocarbons  Carbon Oxides  Gases carbon monoxide (CO) and carbon dioxide (CO 2 )  Greenhouse gases  Hydrocarbons  Diverse group of organic compounds that contain only hydrogen and carbon (ex: CH 4 - methane)  Some are related to photochemical smog and greenhouse gases

11. Ozone  Tropospheric Ozone  Man- made pollutant in the lower atmosphere  Secondary air pollutant  Component of photochemical smog  Stratospheric Ozone  Essential component that screens out UV radiation in the upper atmosphere  Man-made pollutants (ex: CFCs) can destroy it

12. Sources of Outdoor Air Pollution  Two main sources  Transportation  Industry  Intentional forest fires is also high

13. Urban Air Pollution  Photochemical Smog (ex: Los Angeles below)  Brownish-orange haze formed by chemical reactions involving sunlight, nitrogen oxide, and hydrocarbons

14. Formation of Photochemical Smog

15. Sources of Smog in Los Angeles

16. Effects of Air Pollution  Low level exposure  Irritates eyes  Causes inflammation of respiratory tract  Can develop into chronic respiratory diseases

17. Children and Air Pollution  Greater health threat to children than adults  Air pollution can restrict lung development  Children breath more often than adults  Children who live in high ozone areas are more likely to develop asthma

18. Without Electrostatic precipitator With Electrostatic precipitator Controlling Air Pollution  Smokestacks with electrostatic precipitator (right)

19. Controlling Air Pollution  Smokestacks with scrubbers (right)  Particulate material can also be controlled by proper excavating techniques

20. Controlling Air Pollution  Gasoline vapors are a major source of VOC’s (volatile organic compounds), which are extremely harmful!  Phase I Vapor Recovery System for gasoline involves collecting unburned vapors from underground tanks at gas stations!

21. The Clean Air Act  Authorizes EPA to set limits on amount of specific air pollutants permitted  Focuses on 6 pollutants:  lead, particulate matter, sulfur dioxide, carbon monoxide, nitrogen oxides, and ozone  Act has led to decreases

22. The Clean Air Act

23. Urban Air Quality

24. Other Ways to Improve Air Quality  Reduce sulfur content in gasoline from its current average of 330 ppm to 30 ppm  Sulfur clogs catalytic converters  Require federal emission standards for all passenger vehicles  Including SUVs, trucks and minivans  Require emission testing for all vehicles  Including diesel

25. Ozone Depletion in Stratosphere  Ozone Protects earth from UV radiation

26. Stratospheric Ozone: Ozone (O 3 ) forms a layer in the stratosphere, measured in Dobson Units (typically 260 DU near the equator, higher toward the poles) Ozone is created when UV radiation strikes molecules of Oxygen (O 2 ) in the stratosphere, and splits (dissociates) them into free O atoms, which then quickly combine to form ozone. 1. 1. O 2 + UV -> O + O 2. 2. O + O 2 -> O 3

27. Stratospheric Ozone: Ozone can then be destroyed & reformed by the same UV radiation, in a natural cycle as follows: 3. 3. O 3 + UV -> O 2 + O 4. 4. O + O 2 -> O 3 as above   Ozone levels peak at about 25 KM above Earth’s surface.   Stratospheric Ozone – absorbs 99% of UV if left at “natural” levels

28. Three Categories of UV Radiation: UV-CUV-BUV-A Size of Wavelength: 200-280280-320320-400 Absorption: Fully absorbed by O2 & O3 Most is absorbed by O3 Mostly reaches surface Results Associated with Exposure: Serious cell mutation, cancer Skin cancer & cataracts, phytoplankton kills Produces Vitamin D with background exposure levels

29. Ozone Depletion in Stratosphere Ozone thinning/hole  First identified in 1985 over Antarctica  Caused by human-produced bromine and chlorine containing chemicals. (Halogens)  Ex: CFCs  propellants used for aerosol cans (no longer in use)  coolants in refrigeration (Freon)  foam (Styrofoam)  blowing agents in insulation  solvents

30. How does Chlorine (CFC) destroy Ozone? Chemical reaction creates a catalyst! 1. 1. CCl 3 F + UV Cl + CCl 2 F 2. 2. Cl + O 3 ClO + O 2 3. 3. ClO + O Cl + O 2

31. Ozone Depletion in Stratosphere  Hole over Antarctica requires three conditions:  The development of the circumpolar vortex - a mass of frigid air that circulates around the southern polar region  The formation of polar stratospheric clouds – masses of ice crystals onto which Cl and Br can settle. This enables Cl and Br to destroy ozone  Sunlight just returning to polar region (occurs in spring in the S. hemisphere (Sept. – Oct.) which triggers the release of the Cl and Br from the polar stratospheric clouds

32. Effects of Ozone Depletion  Higher levels of UV- radiation hitting the earth  Eye cataracts  Skin cancer (right)  Weakened immunity  May disrupt ecosystems  May damage crops and forests

33. Recovery of Ozone Layer  Montreal Protocol (1987)  Reduction of CFCs  Started using HCFCs (greenhouse gas)  Phase out of all ozone destroying chemicals is underway globally  Satellite pictures in 2000 indicated that ozone layer was recovering  Full recovery will not occur until 2050

34. Acid Deposition  Sulfur dioxide and nitrogen dioxide emissions react with water vapor in the atmosphere and form acids that return to the surface as either dry or wet deposition  pH scale

35. How Acid Deposition Develops

36. Effects of Acid Deposition  Declining Aquatic Animal Populations  Thin-shelled eggs prevent bird reproduction  Calcium is unavailable in acidic soil  Forest decline

37. Acid Deposition and Forest Decline

38. Air Pollution Around the World  Air quality is deteriorating rapidly in developing countries  Developing countries have older cars  Shenyang, China  Residents only see sunlight a few weeks each year  5 worst cities in world  Beijing, China;  Mexico City, Mexico;  Shanghai, China;  Tehran, Iran;  Calcutta, India

39. Case-In-Point Air Pollution in Beijing and Mexico City  Beijing (left)  Mexico City (above)

40. Global Distillation Effect Long Distance Transport of Air Pollutants

41. Indoor Air Pollution  Pollutants can be 5-100X greater than outdoors  Radon, cigarette smoke, carbon monoxide, nitrogen dioxide, formaldehyde pesticides, lead, cleaning solvents, ozone, and asbestos

42. Indoor Air Pollution - Radon