Worlds in the making: The evolution of the universeArrhenius, Svante
Science
Worlds in the making: The evolution of the universe
Arrhenius, Svante
Cosmogony
Our considerations lead to the conclusion that there is rotating about
the central body of the nebula an immense mass of gas, and that outside
this mass there are other centres of condensation moving about the
central body together with the masses of gas concentrated about them.
Owing to the friction between the immigrated masses and the original
mass of gas which circulated in the equatorial plane of the central
body, all these masses will keep near the equatorial plane, which will
therefore deviate little from the ecliptic. We thus obtain a proper
planetary system, in which the planets are surrounded by colossal
spheres of gas like the stars in the Pleiades (Fig. 52). If, now, the
planets have very small mass by comparison with the central body—as
in our solar system—they will be cooled at an infinitely faster rate
than the sun. The gaseous masses will soon shrink, and the periods of
rotation will be shortened; but for those planets, at least, which are
situated near the centre, these periods will originally differ little
from the rotation of the central body. The dimensions of the central
body will always be very large, and the planets circulating about it
will produce very strong tidal effects in its mass. Its period of
rotation will be shortened, while the orbital rotation of the planets
will tend to become lengthened. Thus the equilibrium is disturbed;
it is re-established again, because the planet is, so to say, lifted
away from the sun, as G. H. Darwin has so ingeniously shown with
regard to the moon and the earth. Similar relations will prevail in
the neighborhood of those planets which will thus become provided with
moons. Hence we understand the peculiar fact that all the planets move
almost in the same plane, the so-called ecliptic, and in approximately
circular orbits; that they all move in the same direction, and that
they have the same direction of rotation in common with their moons and
with the central body, the sun. It is only the outermost planets, like
Uranus and Neptune, in whose cases the tidal effects were not of much
consequence, that form exceptions to this rule.
In explanation of these phenomena various philosophers and astronomers
have advanced a theory which is known as the Kant-Laplace theory,
after its most eminent advocates. Suggestions pointing in the same
direction we find in Swedenborg (1734). Swedenborg assumed that our
planetary system had been evolved under the formation of vortices from
a kind of “chaos solare,” which had acquired a more and more energetic
circulating motion about the sun under the influence of internal
forces, possibly akin to magnetic forces. Finally a ring had been
thrown off from the equator, and had separated into fragments, out of
which the planets had been formed.
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