Page 56 - Fundamentals of Air Pollution
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32               2. The Natural versus Polluted Atmosphere



















                   Fig. 2-5. Transport and diffusion from source to receptor.




       straight line between the source and the receptor, but may meander some-
       what about that line as wind direction fluctuates from its mean value over
       the time of transit between the two points)—tend to make the concentration
       of the plume as it arrives at the receptor less than its concentration on
       release from the stack. The sum of all these processes is called diffusion.
       The process of diffusion becomes increasingly complex as the number of
       sources and receptors increases; as sources and receptors begin to group
       together into towns and cities; as some of the sources and receptors move,
       e.g., vehicles; and, finally, as the weather and topography become more
       complex than a wind blowing in one direction over a flat desert for a
       prolonged period of time.
         If the plume being transported is above the height where ground-based
       convective and turbulent processes will bring it down to the ground reason-
       ably close to its origin, it may travel for hundreds of miles at that height
       before being brought to earth, by these processes, in a remote community.
       This is known as long-range or long-distance transport.

       D. Significant Deterioration of Air Quality
       It may be desirable to curtail transport of pollution to areas whose air is
       presently quite clean, even though, after such transport, the air quality of
       the area would be considerably cleaner than would be required by air quality
       standards. This concept is called prevention of significant deterioration of
       the air quality in such areas. It requires definition of how much deterioration
       can be considered insignificant.

       E. Polluted Atmosphere
         Sections II and III describe the types and form of gases, vapors, and
       particles in the atmosphere. Definitions of terms are offered at the beginning
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