Meteoric astronomy: A treatise on shooting-stars, fire-balls, and aerolitesKirkwood, Daniel
Science
Meteoric astronomy: A treatise on shooting-stars, fire-balls, and aerolites
Kirkwood, Daniel
Meteors
With respect to meteorites the same author remarks that "like the
moon, they are probably satellites of the earth; but being very small,
they are liable to extraordinary perturbations, and hence strike the
earth in many directions." Here, again, his _facts_ are at fault; for
(1) the observed velocities of these bodies are inconsistent with the
supposition of their being satellites of the earth; and (2) the amount
of perturbation of such bodies does not vary with their masses: a
_small_ meteorite would fall toward the earth or any other planet with
no greater velocity than a _large_ one.
THE METEORIC THEORY.
It has been shown in a previous chapter that immense numbers of
meteoric asteroids are constantly traversing the planetary spaces--that
many millions, in fact, daily enter the earth's atmosphere. Reasons
are not wanting for supposing the numbers of these bodies to increase
with great rapidity as we approach the center of the system. Moreover,
on account of the greater force of gravity at the sun's surface the
heat produced by their fall must be much greater than at the surface
of the earth. It has been calculated that if one of these asteroids
be arrested in perihelion by the solar atmosphere, the quantity of
heat thus developed will be 9000 times greater than that produced by
the combustion of an equal mass of coal. There can, therefore, be no
reasonable doubt that a _portion_ of the sun's heat is produced by
the impact of meteoric matter. In considering the probability that it
is _chiefly_ so generated, the following questions naturally present
themselves:
1. _What amount of matter precipitated upon the sun would develop
the quantity of heat actually emitted?_--This question has been
satisfactorily discussed by eminent physicists, and it will be
sufficient for our purpose to give the result. According to Professor
William Thomson, of Glasgow, the present rate of emission would be kept
up by a meteoric deposit which would form an annual stratum 60 feet in
thickness over the sun's surface.
2. _Could such an increase of the sun's magnitude be detected by
micrometrical measurement?_--This inquiry is readily answered in the
negative. The apparent diameter would be augmented only one second in
17,600 years.
3. _Is there any known or visible source from which this amount
of meteoric matter may be supplied?_--Thomson, Mayer, and other
distinguished writers regard the zodiacal light as the source of
such meteorites. The inner portions of this immense "tornado" must
be resisted in their motions by the solar atmosphere, and hence
precipitated upon the sun's surface.
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