Scientific American Supplement, No. 455, September 20, 1884 — John Shaqi
Scientific American Supplement, No. 455, September 20, 1884Various
Science
Scientific American Supplement, No. 455, September 20, 1884
Various
Science -- Periodicals
Returning to the discussion of the state of affairs existing when the
particles have reached their highest position in the atmosphere, we may
imagine that they set themselves off on journeys toward either the north
or the south pole. As they pass from the hotter to the colder regions, a
number of particles coalesce; these again combine with others on the road
until the vapor becomes visible as cloud. The increased density implies
increased weight, and the cloud particles, as they sail poleward, descend
toward the surface of the earth. Assuming that a spherical form is
maintained throughout, the condensation of a number of particles implies a
considerable reduction of surface. Thus, the contents of two spheres vary
as the cubes of their radii, or eight (the cube of 2) drops on combining
will form a drop twice the radius of one of the original drops. We may
safely conceive hundreds and thousands of such combinations to take place
until a cloud mass is formed, in which the constituent parts are more or
less in contact, and, therefore, behave electrically as a single conductor
of irregular surface, upon which is accumulated all the electricity that
was previously distributed over the surfaces of the millions of particles
that now compose it.
The tendency of an electric charge upon the surface of a conductor is to
take upon itself a position in which it may approach nearest to an equal
and opposite charge; or, if possible, to attain neutrality. If, then, a
cloud has a charge, and there is no other cloud above or near it, the
charge _induces_ on the adjacent earth surface electricity of the opposite
kind. Thus, assuming the cloud to be charged with positive electricity,
the subjacent earth will be in the negative state. The two
electricities[3] exert a strong tendency to combine or to produce
neutrality, whence there is a species of stress applied to the intervening
air. Possibly the cloud will be drawn bodily toward the earth more or less
rapidly, according as the charge is great or small. Or, on the other hand,
the cloud may roll on for leagues, carrying its influence with it, so that
the various portions of the earth underneath become successively charged
and discharged as the cloud progresses on its journey.
[Footnote 3: We may speak of two electricities or two electric states
without necessarily implying adherence either to the single or the double
"fluid" theory. Whether electricity be of two kinds or no, the fact
remains that there are two conditions, and all the features of this paper
may be explained with equal facility by the supporters of either
hypothesis.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account