The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
In this dynamical principle we have in all probability a physical
explanation of that remarkable characteristic of celestial movements to
which we have referred. The solar system possesses less energy in
proportion to its moment of momentum than it would require to have if
the orbits of the important planets, instead of lying practically in the
same plane, were inclined at various angles. Whatever may have been the
original disposition of the materials forming the solar system, they
must once have contained much more energy than they have at present. The
moment of momentum in the principal plane, at the beginning, was not,
however, different from the moment of momentum that the system now
possesses. As the energy of the system gradually declined, the system
has gradually been compelled to adjust itself in such a manner that,
with the reduced quantity of energy, the requisite moment of momentum
shall still be preserved. This is the reason why, in the course of the
myriads of ages during which the solar system has been acquiring its
present form, the movements have gradually become nearly conformed to a
plane.
The operation of the principle, now before us, may be seen in a striking
manner in Saturn’s ring. (Fig. 37.) The particles constituting this
exquisite object, so far as observations have revealed them, seem to
present to us an almost absolutely plane movement. The fact that the
movements of the constituents of Saturn’s ring lie in a plane is
doubtless to be accounted for by the operation of the fundamental
dynamical principle to which we have referred. Saturn, in its great
motion round the luminary, is, of course, controlled by the sun, yet the
system attached to Saturn is so close to that globe as to be attracted
by the sun in a manner which need not here be distinguished from the
solar attraction on Saturn itself. It follows that the differential
action, so to speak, of the sun on Saturn, and on the myriad objects
which constitute its ring, may be disregarded. We are therefore
entitled, as already mentioned, to view Saturn and its system as an
isolated group, not acted upon by any forces exterior to the system. It
is therefore subject to the laws which declare that, though the energy
declines, the moment of momentum is to remain unaltered. This it is
which has apparently caused the extreme flatness of Saturn’s ring. The
energy of the rotation of that system has been expended until it might
seem that no more energy has been left than just suffices to preserve
the unalterable moment of momentum, under the most economical
conditions, so far as energy is concerned.
[Illustration: Fig. 37.—SATURN. Drawn by E. M. Antoniadi. (July 30th,
1899.)]
Public-domain text, read in full here on John Shaqi.
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