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Chapter 19 Air Pollution
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Overview of Chapter 19 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
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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
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Air Pollution - Terminology
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
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Major Air Pollutants
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Major Classes of Air Pollutants
Particulate Material Nitrogen Oxides Sulfur Oxides Carbon Oxides Hydrocarbons Ozone
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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
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Particulates Classification (2.5 vs. 10.0)
Pm 2.5 = combustion particles, metals, organic compounds of 2.5 microns and below Pm 10.0 = larger solid particles (10 microns and above); Typically dust, pollen, mold, etc.
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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
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Carbon Oxides and Hydrocarbons
Gases carbon monoxide (CO) and carbon dioxide (CO2) Greenhouse gases Hydrocarbons (HC’s) Diverse group of organic compounds that contain only hydrogen and carbon (ex: CH4- methane) Some are related to photochemical smog and greenhouse gases
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Ozone Tropospheric Ozone Stratospheric 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
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Ozone Damage to Grape Leaves
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Primary Air Pollutants
NOTE: Ozone is a secondary air pollutant that can be indirectly measured by nitrogen oxides and volatile organics concentrations
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Sources of Outdoor Air Pollution
Two main sources Transportation Industry Intentional forest fires is also high
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Urban Air Pollution Photochemical Smog (ex: Los Angeles below)
Brownish-orange haze formed by chemical reactions involving sunlight, nitrogen oxide, and hydrocarbons
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Formation of Photochemical Smog
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Sources of Smog in Los Angeles
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Effects of Air Pollution
Low level exposure Irritates eyes Causes inflammation of respiratory tract Can develop into chronic respiratory diseases
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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
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Controlling Air Pollution
Smokestacks with electrostatic precipitator (right) Without Electrostatic precipitator With Electrostatic precipitator
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Controlling Air Pollution
Smokestacks with scrubbers (right) Particulate material can also be controlled by proper excavating techniques
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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!
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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
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The Clean Air Act
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Urban Air Quality
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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
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Ozone Depletion in Stratosphere
Ozone Protects earth from UV radiation
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Stratospheric Ozone: Ozone (O3) 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 (O2) in the stratosphere, and splits (dissociates) them into free O atoms, which then quickly combine to form ozone. O2 + UV -> O + O O + O2 -> O3
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Stratospheric Ozone: Ozone can then be destroyed & reformed by the same UV radiation, in a natural cycle as follows: O3 + UV -> O2 + O O + O2 -> O3 as above Ozone levels peak at about 25 KM above Earth’s surface. Stratospheric Ozone – absorbs 99% of UV if left at “natural” levels
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Three Categories of UV Radiation:
UV-C UV-B UV-A Size of Wavelength: (nm) 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
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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
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How does Chlorine (CFC) destroy Ozone?
Chemical reaction creates a catalyst! CCl3F + UV Cl + CCl2F Cl + O ClO + O2 ClO + O Cl + O2
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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
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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
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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 or later
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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
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How Acid Deposition Develops
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Effects of Acid Deposition
Declining Aquatic Animal Populations Thin-shelled eggs prevent bird reproduction Calcium is unavailable in acidic soil Forest decline
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Acid Deposition and Forest Decline
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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
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Case-In-Point Air Pollution in Beijing and Mexico City
Beijing (left) Mexico City (above)
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Long Distance Transport of Air Pollutants
Global Distillation Effect
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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
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Indoor Air Pollution - Radon
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