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Ozone: Good Up
High, Bad Nearby
Ozone is a gas that forms in the
atmosphere when 3 atoms of oxygen are combined (03). It is not
emitted directly into the air, but at ground level is created by a chemical
reaction between oxides of nitrogen (NOx), and volatile organic
compounds (VOC) in the presence of sunlight. Ozone has the same chemical
structure whether it occurs high above the earth or at ground level and can be
"good" or "bad," depending on its location in the
atmosphere.
How Can Ozone Be Both
Good and Bad?
Ozone
occurs in two layers of the atmosphere. The layer surrounding the earth's
surface is the troposphere. Here, ground-level or "bad" ozone is an
air pollutant that damages human health, vegetation, and many common
materials. It is a key ingredient of urban smog. The troposphere extends to a
level about 10 miles up, where it meets the second layer, the stratosphere.
The stratospheric or "good" ozone layer extends upward from about 10
to 30 miles and protects life on earth from the sun's harmful ultraviolet rays
(UV-b).
Ozone
occurs naturally in the stratosphere and is produced and destroyed at a
constant rate. But this "good" ozone is gradually being destroyed by
manmade chemicals called chlorofluorocarbons (CFCs), halons, and other ozone
depleting substances (used in coolants, foaming agents, fire extinguishers,
and solvents). These ozone depleting substances degrade slowly and can remain
intact for many years as they move through the troposphere until they reach
the stratosphere. There they are broken down by the intensity of the sun's
ultraviolet rays and release chlorine and bromine molecules, which destroy
"good" ozone. One chlorine or bromine molecule can destroy 100,000
ozone molecules, causing ozone to disappear much faster than nature can
replace it.
It can take years for ozone depleting
chemicals to reach the stratosphere, and even though we have reduced or
eliminated the use of many CFCs, their impact from years past is just starting
to affect the ozone layer. Substances released into the air today will
contribute to ozone destruction well into the future.
Satellite observations indicate a
world-wide thinning of the protective ozone layer. The most noticeable losses
occur over the North and South Poles because ozone depletion accelerates in
extremely cold weather conditions.
As the stratospheric ozone layer
is depleted, higher UV-b levels reach the earth's surface. Increased UV-b can
lead to more cases of skin cancer, cataracts, and impaired immune systems.
Damage to UV-b sensitive crops, such as soybeans, reduces yield. High altitude
ozone depletion is suspected to cause decreases in phytoplankton, a plant that
grows in the ocean. Phytoplankton is an important link in the marine food
chain and, therefore, food populations could decline. Because plants
"breathe in" carbon dioxide and "breathe out" oxygen,
carbon dioxide levels in the air could also increase. Increased UV-b radiation
can be instrumental in forming more ground-level or "bad" ozone.
The Montreal Protocol, a series
of international agreements on the reduction and eventual elimination of
production and use of ozone depleting substances, became effective in 1989.
Currently, 160 countries participate in the Protocol. Efforts will result in
recovery of the ozone layer in about 50 years.
In the United States, the U.S.
Environmental Protection Agency (EPA) continues to establish regulations to
phase out these chemicals. The Clean Air Act requires warning labels on all
products containing CFCs or similar substances, prohibits nonessential ozone
depleting products, and prohibits the release of refrigerants used in car and
home air conditioning units and appliances into the air.
What Causes "Bad" Ozone?
Motor vehicle exhaust and
industrial emissions, gasoline vapors, and chemical solvents are some of the
major sources of NOx and VOC, also known as ozone precursors.
Strong sunlight and hot weather cause ground-level ozone to form in harmful
concentrations in the air. Many urban areas tend to have high levels of
"bad" ozone, but other areas are also subject to high ozone levels
as winds carry NOx emissions hundreds of miles away from their
original sources.
Ozone concentrations can vary from year
to year. Changing weather patterns (especially the number of hot, sunny days),
periods of air stagnation, and other factors that contribute to ozone
formation make long-term predictions difficult.
Repeated exposure to ozone
pollution may cause permanent damage to the lungs. Even when ozone is present
in low levels, inhaling it triggers a variety of health problems including
chest pains, coughing, nausea, throat irritation, and congestion. It also can
worsen bronchitis, heart disease, emphysema, and asthma, and reduce lung
capacity.
Healthy people also experience
difficulty in breathing when exposed to ozone pollution. Because ozone
pollution usually forms in hot weather, anyone who spends time outdoors in the
summer may be affected, particularly children, the elderly, outdoor workers
and people exercising. Millions of Americans live in areas where the national
ozone health standards are exceeded.
Ground-level ozone damages plant life
and is responsible for 500 million dollars in reduced crop production in the
United States each year. It interferes with the ability of plants to produce
and store food, making them more susceptible to disease, insects, other
pollutants, and harsh weather. "Bad" ozone damages the foliage of
trees and other plants, ruining the landscape of cities, national parks and
forests, and recreation areas.
What is
Being Done About Bad Ozone?
The
Clean Air Act Amendments of 1990 require EPA, states, and cities to implement
programs to further reduce emissions of ozone precursors from sources such as
cars, fuels, industrial facilities, power plants, and consumer/commercial
products. Power plants will be reducing emissions, cleaner cars and fuels are
being developed, many gas stations are using special nozzles at the pumps to
recapture gasoline vapors, and vehicle inspection programs are being improved
to reduce emissions.
The ultimate responsibility for our
environment is our own. Minor lifestyle changes can result in major air
quality improvements.
What Can You Do?
High-Altitude "Good" Ozone
- Make sure that technicians working on
your car air conditioner, home air conditioner, or refrigerator are
certified by an EPA approved program to recover the refrigerant (this is
required by law).
- Have your car and home air
conditioner units and refrigerator checked for leaks. When possible,
repair leaky air conditioning units before refilling them.
- Contact local authorities to properly
dispose of refrigeration or air conditioning equipment.
- Protect yourself against sunburn.
Minimize sun exposure during midday hours (10 am to 4 pm). Wear
sunglasses, a hat with a wide brim, and protective clothing with a tight
weave. Use a broad spectrum sunscreen with a sun protection factor (SPF)
of at least 15 and 30 is better.
Ground-Level "Bad"
Ozone
- Keep your automobile well tuned and
maintained.
- Carpool, use mass transit, walk,
bicycle, and/or reduce driving, especially on hot summer days.
- Be careful not to spill gasoline when
filling up your car or gasoline-powered lawn and garden equipment. During
the summer, fill your gas tank during the cooler evening hours.
- Make sure your car's tires are properly
inflated and your wheels are aligned.
- Participate in your local utility's
energy conservation programs.
- Seal containers of household cleaners,
workshop chemicals and solvents, and garden chemicals to prevent VOC from
evaporating into the air. Dispose of them properly.
We live with
ozone every day. It can protect life on earth
or harm it, but we have the power to influence
ozone's impact by the way we live.
U.S. Environmental Protection Agency
For more information visit
the Stratospheric Ozone website at http://www.epa.gov/ozone
Also visit EPA's Office of Air and Radiation website at http://www.epa.gov/oar/
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High, Bad Nearby
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