Classics of modern science : $b (Copernicus to Pasteur)
History
Classics of modern science : $b (Copernicus to Pasteur)
Science; Science -- History
If all the particles of a ring of vapours continued to condense without
separating, they would at length constitute a solid or a liquid ring.
But the regularity which this formation requires in all the parts of
the ring, and in their cooling, ought to make this phenomenon very
rare. Thus the solar system presents but one example of it; that of the
rings of Saturn. Almost always each ring of vapours ought to be divided
into several masses, which, being moved with velocities which differ
little from each other, should continue to revolve at the same distance
about the Sun. These masses should assume a spheroidical form, with a
rotatory motion in the direction of that of their revolution, because
their inferior particles have a less real velocity than the superior;
they have therefore constituted so many planets in a state of vapour.
But if one of them was sufficiently powerful, to unite successively by
its attraction, all the others about its centre, the ring of vapours
would be changed into one sole spheroidical mass, circulating about
the Sun, with a motion of rotation in the same direction with that
of revolution. This last case has been the most common; however, the
solar system presents to us the first case, in the four small planets
which revolve between Mars and Jupiter, at least unless we suppose
with Olbers, that they originally formed one planet only, which was
divided by an explosion into several parts, and actuated by different
velocities. Now if we trace the changes which a further cooling ought
to produce in the planets formed of vapours, and of which we have
suggested the formation, we shall see to arise in the centre of each
of them, a nucleus increasing continually, by the condensation of the
atmosphere which environs it. In this state, the planet resembles the
Sun in the nebulous state, in which we have first supposed it to be;
the cooling should therefore produce at the different limits of its
atmosphere, phenomena similar to those which have been described,
namely, rings and satellites circulating about its centre in the
direction of its motion of rotation, and revolving in the same
direction on their axes. The regular distribution of the mass of rings
of Saturn about its centre and in the plane of its equator, results
naturally from this hypothesis, and, without it, is inexplicable. Those
rings appear to me to be existing proofs of the primitive extension of
the atmosphere of Saturn, and of its successive condensations. Thus,
the singular phenomena of the small eccentricities of the orbits of the
planets and satellites, of the small inclination of these orbits to the
solar equator, and of the identity in the direction of the motions of
rotation and revolution of all those bodies with that of the rotation
of the Sun, follow the hypothesis which has been suggested, and render
it extremely probable. If the solar system was formed with perfect
regularity, the orbits of the bodies which compose it would be circles,
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