Air Pollution and Stratospheric Ozone Depletion

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Air Pollution and Stratospheric Ozone Depletion
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Air Pollution and Stratospheric Ozone Depletion Chapter 15 Air Pollution and Stratospheric Ozone Depletion

Chattanooga Tennessee. Along a natural basin of the Appalachian mountains. After civil war, became a leading manufacturing center in the nation. 1957-3rd worst particulate pollution in the nation. 1969 (year before CAA)-created its own air pollution legislation (Air pollution Control Ordinance). City and County also put new pollution monitoring techniques. $40 million in cleanup efforts.

1972- Chattanooga meets compliance with the CAA quality standards. To maintain their clean air: Comprehensive recycling program. Largest municipal fleet of electric buses in the US. Despite efforts, Ozone concentrations exceeded the 1997 standard. Chattanooga made the efforts again to comply through combined government, public, and local industry efforts.

Air Pollution Air pollution- the introduction of chemicals, particulate matter, or microorganisms into the atmosphere at concentrations high enough to harm plants, animals, and materials such as buildings, or to alter ecosystems. Sources can be natural such as volcanoes and fires or anthropogenic like automobiles and factories. Air pollution doesn’t stay local: Acid rain rainfall on the west coast of the US has been caused by pollution in Asia.

Major Air Pollutants CAA 1970 identified 6 pollutants that significantly threaten human well-being. Criteria air pollutants. Sulfur Dioxide Nitrogen Oxides Carbon monoxide (dioxide listed in 2007. US supreme court rule) Particulate Matter Ozone Lead Other air pollutants Mercury Volatiles Organic Compounds

Primary Pollutants Primary pollutants- polluting compounds that come directly out of the smoke-stack, exhaust pip, or natural emission source. Examples: CO, CO2, SO2, NOx, and most suspended particulate matter.

Secondary Pollutants Secondary pollutants- pollutants that have undergone transformation in the presence of sunlight, water, oxygen, or other compounds. Examples: ozone, sulfate and nitrate

Natural Sources of Air Pollution Volcanoes Lightning Forest fires Plants

Anthropogenic Sources of Air Pollution On-road vehicles Power plants Industrial processes Waste disposal

Deposit within the respiratory system and are usually more toxic.

Los Angeles Type: Brown Smog Photochemical Smog Los Angeles Type: Brown Smog London type: Gray Smog

Temperature Atmospheric temperature affects the formation of smog. Evaporation of VOC’s increase as the temperature increases. NOx emissions from electric utilities also increase as air- conditioning demands increase. Chemical reactions that form ozone proceed more rapidly at higher temperatures These factors combine to form even higher smog concentrations…positive feedback loop.

Thermal Inversions Thermal Inversion- when a relatively warm layer of air at mid-altitude covers a layer of cold, dense air below. The warm inversion layer traps emissions that then accumulate beneath it.

Acid Deposition All rain is slightly acidic. pH’s less than 5.6 are considered acid deposition. Pollutants combine with water & oxygen in atmosphere with primary pollutants to form sulfuric acid and nitric acid.

Acid Deposition Acid deposition- occurs when nitrogen oxides and sulfur oxides are released into the atmosphere and combine with atmospheric oxygen and water. These form the secondary pollutants nitric acid and sulfuric acid. Acid deposition increased substantially in the US from the 1940’s-1990’s due to human activity. These secondary pollutants further break down into nitrate and sulfate which cause the acid in acid deposition.

Effects of Acid Deposition Direct effects Indirect effects Lowering the pH of lake water Damaging statues, monuments, and buildings Mobilizing metals that are found in soils and releasing these into surface waters Decreasing species diversity of aquatic organisms

Ways to Prevent Air Pollution Removing sulfur dioxide from coal by fluidized bed combustion. (using less fuel: Better) Catalytic converters on cars Scrubbers on smoke stacks Baghouse filters Electrostatic precipitators

Bag house filter

Electrostatic precipitator

Scrubber

Stratospheric Ozone The stratospheric ozone layer exists roughly 45-60 kilometers above the Earth. Ozone has the ability to absorb ultraviolet radiation and protect life on Earth.

Formation and Breakdown of Ozone First, UV-C radiation breaks the bonds holding together the oxygen molecule )2, leaving two free oxygen atoms: O2 + UV-C -> 2O Sometimes the free oxygen atoms result in ozone: O2 + O -> O3 Ozone is broken down into O2 and free oxygen atoms when it absorbs both UV-C and UV-B ultraviolet light: O3 + UV-B or UV-C -> O2 + O

Anthropogenic Contributions to Ozone Destruction Certain chemicals can break down ozone, particularly chlorine. The major source of chlorine in the stratosphere is a compound known as chlorofluorocarbons (CFCs) CFCs are used in refrigeration and air conditioning, as propellants in aerosol cans and as “blowing agents” to inject air into foam products like Styrofoam.

Anthropogenic Contributions to Ozone Destruction When CFCs are released into the troposphere they make their way to the stratosphere. The ultraviolet radiation present has enough energy to break the bond connecting chlorine to the CFC molecule. which can then break apart the ozone molecules.

Anthropogenic Contributions to Ozone Destruction First, chlorine breaks ozone’s bonds and pulls off one atom of oxygen, forming a chlorine monoxide molecule and O2: O3 + Cl -> ClO + O2 Next, a free oxygen atoms pulls the oxygen atom from ClO, liberating the chlorine and creating one oxygen molecule: ClO + O -> Cl + O2 One chlorine atom can catalyze the breakdown of as many as 100,000 ozone molecules before it leaves the stratosphere.

Depletion of the Ozone Layer Global Ozone concentrations had decreased by more than 10%. Depletion was greatest at the poles Decreased stratospheric ozone has increased the amount of UV-B radiation that reaches the surface of Earth.

Indoor Air Pollutants Causes more deaths per year than outdoor. 1.6 million deaths worldwide: 56% in ages of 5 or less. Developing countries Developed countries Wood, animal manure or coal used for cooking and heating in developing countries. CO and PM’s Acute respiratory infections, pneumonia, bronchitis, cancer. More time in doors, better insulation, building materials made from petroleum and plastics that give off vapors. Asbestos Carbon Monoxide Radon VOCs in home products

80-90% of our time is spent indoors.