Scientific American Supplement, No. 455, September 20, 1884Various
Science
Scientific American Supplement, No. 455, September 20, 1884
Various
Science -- Periodicals
It is possible, however, with the aid of our knowledge of static
electricity, to arrive at hypotheses of a more than chimerical nature. In
the first place, that our sphere is a more or less electrified body is
generally admitted. More than this, it is demonstrated that the different
parts of the earth's surface and its enveloping atmosphere are variously
charged. As a consequence of these varying charges, there is a constant
series of currents flowing through the various parts of the earth, which
show themselves in such telegraph wires as may lie in the direction
followed by the currents. Such currents are known as earth currents, and
present phenomena of a highly interesting nature. But, apart from these
electrical manifestations, there is generally a difference of electrical
condition between the various parts of the earth's surface and those
portions of the atmosphere adjacent to or above them. Inasmuch as air is
one of the very best insulators, this difference of condition (or
potential) in any particular region is in most cases incapable of being
neutralized or equilibrated by an electric flow. Consequently the air
remains more or less continually charged. With these points admitted as
facts, the question arises, Whence this electricity? There have been very
many and various opinions expressed as to the cause of terrestrial
electricity, but far the greater portion of such theories lack fundamental
probability, and indicate causes which cannot be regarded as sufficiently
extensive or operative to produce such tremendous effects as are
occasionally witnessed. I take it that we may safely regard the evolution
of electricity as one of the ways in which force exhibits itself, that, in
other words, when work is performed electricity may result. When two
bodies are rubbed together, electricity is produced, so also is it when
two connected metals are immersed in water and one of them is dissolved,
or when one of the junctions of two metals is raised to a higher
temperature than the other junction. I will go further than this, so far,
in fact, as to maintain that there is a reasonable ground for supposing
that every movement, whether it be of the mass or among the constituent
particles, is attended by a change of electrical distribution; and if this
is true, it may easily be conceived that inasmuch as motion is the rule of
the universe, there must be a constant series of electrical changes. Now,
these changes do not all operate in one direction, nor are they all of
similar character, whence it is that not only are there earth currents of
feeble electro-motive force, but that this E.M.F. is constantly varying,
and that, furthermore, electricity of high E.M.F. is to be met with in
various parts of the atmosphere.
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