Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
A great many different methods are in use for determining the total
amount of solid matter present in a given volume of air, counting the
number of particles, or gathering samples for microscopic examination.
Thus a known volume of air may be drawn through a filter of cotton
wool or bubbled through distilled water, and the dust detained by the
cotton or deposited in the water may be weighed. In certain types of
apparatus the air is drawn or forced against a plate or tube coated
with glycerin, oil, varnish, gelatin, or other adhesive surface, to
which the dust remains attached. Several devices depend for their
operation upon the fact that when a volume of confined air is cooled
by expansion a point is eventually reached at which the water vapor
present condenses to form a fog, each droplet of which is supposed
to have a single particle of dust as its “nucleus.” This is the
principle involved in the well-known Aitken dust counter, which has
been so extensively used in different parts of the world, and has
furnished most of the impressive statistics of air dustiness found
in textbooks and reference books. Thus, from indications supplied by
this instrument, it is stated that a cubic inch of town air contains
50,000,000 particles of dust; that a room, near the ceiling, was found
to contain 88,000,000 particles per cubic inch; and that a cigarette
smoker sends 4,000,000,000 particles into the air at every puff. Recent
authorities are inclined to look upon these figures as misleading,
for the reason that the nuclei counted with Aitken’s instrument are
probably so infinitesimal in size that they hardly deserve to be called
dust; indeed there is good reason to believe that an indefinitely
large proportion of them may actually be molecules of gases.
Public-domain text, read in full here on John Shaqi.
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