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  • Changes in the atmosphere

    If you were to compare the earth with an

    apple from the supermarket, the atmosphere would be no thicker than the layer of

    shiny wax applied to it. Yet this thin, finite wrapping of air around the planet

    receives more than 700,000 metric tons of pollutants each day in the United

    States alone. Pollutants are substances with which ecosystems have had no prior

    evolutionary experience, in terms of kinds or amounts, and so have no mechanisms

    for dealing with them. From the human perspective, pollutants are substances

    that severely affect our health, activities, or survival.

    Local air

    pollution

    Industrial smog is gray air that predominates in

    industrialized cities with cold, wet winters. London, New York, Pittsburgh, and

    Chicago are examples. These cities use fossil fuel for heating, manufacturing,

    and producing electric power. The burning fuel releases airborne pollutants,

    including dust, smoke, ashes, soot, asbestos, oil, bits of heavy metals, and

    sulfur oxides (硫氧化合物). Industrial smog was the cause of London's 1952 air

    pollution, in which 4,000 people died.

    Photochemical (光化学的) smog is

    brown and smelly trademark of large cities found in warm climates. When the

    surrounding land forms a natural basin, as it does around Los Angeles and Mexico

    city, photochemical smog can reach harmful concentrations. The main component of

    photochemical is nitric oxide (一氧化氮) ,which is produced chiefly by cars and

    other vehicles with internal combustion engines. Nitric oxide reacts with oxygen

    in the air to form nitrogen dioxide(二氧化氮). When exposed to sunlight, nitrogen

    dioxide can react with hydrocarbons to from photochemical oxidant(光化氧化物质). Other

    components of smog are ozone and PANs ( short for peroxyacetyl

    nitrates(硝酸过氧乙酰酯)). PANs are similar to tear gas; even traces can sting the eyes

    and irritate the lungs.

    Acid deposition 1

    Oxides of sulfur(硫磺)

    and nitrogen(氮) are among the most dangerous air pollutant. Coal-burning power

    plants, factories, and metal smelters (金属冶炼厂)are the main sources of sulfur

    dioxides. Vehicles, power plants that burn fossil fuels, and nitrogen

    fertilizers are sources of nitrogen oxides.

    Depending on climatic

    conditions, tiny particles of these substances may be airborne for a while and

    then fall to earth as dry acid deposition. Most sulfur and nitrogen dioxides

    dissolve in atmospheric water to form weak solutions of sulfuric acid and nitric

    acid. Winds can distribute them over great distances before they fall to earth

    in rain or snow; this is called wet acid deposition. Acid rain can be four to

    forty times more acidic than normal rainwater, sometimes as much as lemon juice.

    The acid attack marble, metals, mortar, rubber, plastic, even nylon stockings.

    And they are disrupting ecosystems.

    Researchers confirmed years ago that

    power plants, factories, and vehicles are the main sources of acid deposition,

    and that the depositions are indeed damaging the environment. Not much has been

    done about it. Also, some of the responses to local air pollution standards have

    contributed to the problem, as when very tall smokestack(大烟囱)are added to power

    plants and smelting plants. The idea is to dump acid-laden smoke high in the

    atmosphere so winds can distribute it elsewhere-which winds readily do. The

    world's tallest smokestack, in Sunbury, Ontario, accounts for about one per cent

    of the annual worldwide emission of sulfur dioxide.

    Damage to the ozone

    layer

    The ozone layer in the lower stratosphere (平流层) absorbs most of

    the ultraviolet wavelengths (紫外线的波长) from the sun--a form of radiation that is

    harmful to organisms. Yet this layer has been thinning since 1976. Each spring,

    an ozone "hole" appears over the Antarctic; it extends over an area about the

    size of the continental United States.

    Satellites and high-altitude

    planes have been monitoring the ozone hole since 1978 by 1987, ozone levels

    above Antarctica had declined by fifty per cent--this compared to the previous

    worst case of forty per cent in 1985.

    The reduction in the ozone layer

    is allowing more ultraviolet (紫外线的)radiation to reach the earth's surface, with

    potentially serious and wide-ranging consequences. Already there has been a

    dramatic increase in skin cancers, which almost certainly are related to

    increases in ultraviolet radiation. Contracts (白内障) may become more common, and

    it appears that ultraviolet radiation also can weaken the immune system, making

    individuals more vulnerable to some viral and parasitic(寄生的)infections.

    The cause of ozone reduction are hotly debated in the scientific community, To

    be sure, large volcanic eruption and cyclic(周期的)changes in solar activity have

    some effects. But the prime suspects are chlorofluorocarbons(CFCs氯氟碳), which are

    compounds of chlorine and carbon. These odorless, invisible, and otherwise

    harmless compounds are widely used as propellants in aerosol spray cans,

    collants in refrigerators and conditioners, and industrial solvents; and they

    also are used in making plastic foams, including the Styrofoam cups and cartons

    used for packaging foods, drinks, and other consumer goods.

    An

    international group assembled by the United Nations Environment Program agreed

    to a draft treaty to halve CFC emissions by the year 1999. Most nations seem

    certain to ratify (承认,批准) its provisions. The treaty is a step in the right

    direction, although some feel that it is too little and too late. CFCs already

    in the air will be there for over a century, before natural processes eutralize

    them. You, your children, and your grandchildren will be living with their

    destructive effects. Think about that, the next time you carry a Styrofoam

    container (泡沫塑料饭盒) from a fast-food restaurant.