Directions: prepare for submission the following exercise. Using either slate and stylus, Perkins brailler, or one of the electronic braille software packages, transcribe into braille the following reading on tropospheric ozone. Electronic braille generated using a six-key Perkins emulator is the preferred format.
For your submission, use the following format: Print or type, in braille, your name, email, and institution in the top right-hand corner in the first space, with runovers in Cell Three. Begin brailling on Line Five.
Submit your braille either via email (if you are using one of the computer-based brailling tools). Electronic braille (Mac/PCBrailler, Duxbury, Edgar, Megadots, Pokadots) should be sent via email to rbroadnax@shodor.org. You can also use the text box at the bottom of this page to submit your work. Simply cut and paste the braille into the box, then click on the "Submit braille" button.
No hardcopy braille is accepted. All submissions must be done electronically, using any of the braille preparation software packages (Duxbury, Megadots, Edgar, Pokadot, etc.)
Specific weather conditions are required to convert ozone precursors into ozone. Strong sunlight, high temperatures
and stable air masses provide ideal conditions for the formation of ozone. Sunlight is needed to initiate ozone
formation, and high temperatures (above 90 degrees) increase the rates of the chemical reactions that form ozone. This
helps explain why smog and ozone levels peak during the summer. The number of days with maximum temperature
exceeding 90 degrees Fahrenheit is sometimes used to predict the number of days with high ozone levels. Fluctuations
in an area's ozone level can be attributed partially to variations in regional weather conditions.
Atmospheric circulation usually prevents smog from settling. However, stagnant air masses keep ozone from
dissipating, creating the potential for serious smog conditions. Sometimes ozone and other pollutants are trapped near
the ground by a temperature inversion; a stable layer of cold air trapped under a layer of warmer, less dense air. Rain
often improves air quality by both "raining out" pollutants and cooling air temperatures. Often, ozone and ozone
precursors produced in one area are transported by winds to another area. For example, pollutants formed in New
York City may show up as elevated ozone levels in rural Maine. Geographical conditions, such as mountains, valleys,
and bodies of water may also have an effect on the transport of pollutants. For example, mountains often block the
transport of air so that stagnant air remains in the valley (as in the Los Angeles basin). In coastal areas, land and sea
breezes may transport pollutants offshore during the afternoon (when the land is warmer than the sea) and onshore
during the evening (when the sea is warmer than the land).
As we've mentioned several times, ozone is a powerful oxidant. Oxidants cause redox chemical reactions in which one
substance is broken down (e.g., iron rusts, silver tarnishes, fabric colors fade) -- usually by the breaking of a chemical
bond and the formation of a new bond containing oxygen. When ozone oxidizes another substance, one of the oxygen
atoms in ozone chemically combines with that substance, and the ozone is converted to oxygen.
Ozone has widespread harmful effects on the health of humans and animals, vegetation, and materials.
Ozone, like many other oxidants, irritates the mucous membranes of the respiratory system, causing coughing, nausea,
shortness of breath, pulmonary congestion, and impaired lung function. It aggravates chronic respiratory diseases, such
as asthma and bronchitis, and can cause serious health problems for people in weakened health and the elderly.
Peroxyacetyl nitrates (PAN) and other oxidants that accompany ozone are powerful eye irritants. Exposure for 6-7
hours or more reduces lung function significantly in healthy people during periods of even moderate exercise.
Ozone damages the leaves of plants and trees. Some plant species, such as tobacco, spinach, tomatoes and pinto beans,
are especially sensitive. Damaged plants develop necrotic patterns (brown specks that turn yellow) on the upper
surfaces of their leaves. The necrotic patterns on the tobacco strain Bel-W3 may be used as a indicator of ozone levels.
Annually, ozone causes millions of dollars in crop loss. It also causes premature leaf drop in trees and reduced growth
rates.
Ozone reacts easily with organic materials -- causing weakness, cracking, and other chemical changes. Ozone cracks
stretched rubber, reduces the strength of textiles, causes fading in fabrics and dyes (cotton, acetate, nylon, polyester),
and causes premature cracking in paint.
Photochemical oxidants were first noticed in the early 1940s in Los Angeles. By 1960, photochemical smog had been
identified as a national problem. In 1963 the first Clean Air Act authorized the Public Health Service to study air
pollution and provided training to state and local agencies to control it. The Clean Air Act of 1970 strengthened this
legislation by creating a partnership between state and federal governments. State and local governments became
responsible for preventing and controlling their air pollution. The Environmental Protection Agency (EPA) was
established to set national pollution regulations and standards.
In 1979, the EPA established primary and secondary standards for pollutants called "National Ambient Air Quality
Standards" (NAAQS). Primary standards protect human health while secondary standards protect crops, livestock,
vegetation, and materials. The primary and secondary standards for ozone are 120 parts per billion (ppb). A state is out
of compliance if it exceeds the standard more than one day per year over a three-year average. The Clean Air Act of
1990 requires states to submit "State Implementation Plans" outlining how they will comply with these standards.
Reduction of ground-level ozone is a complicated problem with no easy solution. It will require cooperation between
government, business and individuals. Methods for controlling industrial and automotive emissions include:
conservation, use of alternative fuels, and development of new technologies. Conservation measures include a shift
away from the use of automobiles and toward public transportation, carpooling, bicycling, and walking. Conserving
energy (electricity, heating, air conditioning) also helps, since most of our energy comes from the burning of fossil
fuels (oil, coal, natural gas) that contribute ozone-producing emissions. Alternative fuels include methanol, ethanol,
natural gas (methane), and hydrogen. However, their use runs the risk of solving one problem by creating another.
New technologies will make it possible to reduce fuel consumption and emissions. Through new technology, the sun
could provide non-polluting solar power to heat homes, power cars, or cook meals. The most promising solution to
ozone reduction could be a combination of technological, social, and economic changes.
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