The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
As in the last chapter, where we were dealing with the positions of the
planes of the orbits, there can here be no hesitation as to the true
cause of this most striking characteristic of the planetary movements.
The nebular theory is at once ready with an explanation, as has been
already indicated in Chapter XI. The primæval nebula, endowed in the
beginning with a certain amount of moment of momentum, has been
gradually contracting. It has been gradually expending its energy, as we
have already had occasion to explain; but the moment of momentum has
remained undiminished. And from this it can be shown that the dynamical
principles guiding the evolution of the nebula must ultimately refuse
permission for any planet to revolve in opposition to the general
movement. This point is a very interesting one, and as it is of very
great importance in connection with our system, I must give it some
further illustration and explanation.
The two figures that are shown in Fig. 50 represent two imaginary
systems. We have a sun in each, and we have two planets in each. The sun
is marked with the letter S, and the two planets are designated by A and
B. For simplicity I have represented the orbits as circles, and for the
same reason I have left out the rest of the planets; we shall also
suppose the orbits of the two planets that are involved to lie exactly
in the same plane. In the two systems that I have here supposed, the two
suns are to be of the same weight, the planet A in one system is of
equal mass to the planet A in the other; and the planets B in the two
systems are also equal. It is also assumed that the orbit of A in one
diagram shall be the same as the orbit of A in the other, and that the
orbit of B in one shall be precisely the same as the orbit of B in the
other. The sun rotates in precisely the same manner in both, and takes
the same time for each rotation. A, in one system, goes round in the
same time that A does in the other; and B, in one system, goes round in
the same time that B does in the other. There is, therefore, a perfect
resemblance between the two systems I have here supposed in every point
but one. I have indicated, as usual, the movements of the bodies by
arrows, and, while in one of the systems the sun and A and B all go
round in the same direction, in the other system the sun and A go round,
no doubt, in the same direction, but the direction of B is opposite. We
are not, in this illustration, considering the rotations of the planets
on their axes. That will be dealt with in the next chapter.
[Illustration: Fig. 50.—I. A NATURAL SYSTEM ON THE LEFT.
II. AN UNNATURAL SYSTEM ON THE RIGHT.]
Public-domain text, read in full here on John Shaqi.
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