On the Connexion of the Physical Sciences — John Shaqi
On the Connexion of the Physical SciencesSomerville, Mary
Science
On the Connexion of the Physical Sciences
Somerville, Mary
Physical sciences; Science
With the exception of these two elements, it appears that all the bodies
are in motion, and every orbit in a state of perpetual change. Minute as
these changes are, they might be supposed to accumulate in the course of
ages, sufficiently to derange the whole order of nature, to alter the
relative positions of the planets, to put an end to the vicissitudes of
the seasons, and to bring about collisions which would involve our whole
system, now so harmonious, in chaotic confusion. It is natural to
inquire, what proof exists that nature will be preserved from such a
catastrophe? Nothing can be known from observation, since the existence
of the human race has occupied comparatively but a point in duration,
while these vicissitudes embrace myriads of ages. The proof is simple
and conclusive. All the variations of the solar system, secular as well
as periodic, are expressed analytically by the sines and cosines of
circular arcs (N. 76), which increase with the time; and, as a sine or
cosine can never exceed the radius, but must oscillate between zero and
unity, however much the time may increase, it follows that when the
variations have accumulated to a maximum by slow changes, in however
long a time, they decrease, by the same slow degrees, till they arrive
at their smallest value, again to begin a new course; thus for ever
oscillating about a mean value. This circumstance, however, would be
insufficient, were it not for the small excentricities of the planetary
orbits, their minute inclinations to the plane of the ecliptic, and the
revolutions of all the bodies, as well planets as satellites, in the
same direction. These secure the perpetual stability of the solar system
(N. 77). However, at the time that the stability was proved by La Grange
and La Place, the telescopic planets between Mars and Jupiter had not
been discovered; but La Grange, having investigated the subject under a
very general point of view, showed that, if a planetary system be
composed of very unequal masses, the whole of the larger would maintain
an unalterable stability with regard to the form and position of their
orbits, while the orbits of the lesser might undergo unlimited changes.
M. Le Verrier has applied this to the solar system, and has found that
the orbits of all the larger planets will for ever maintain an
unalterable stability in form and position; for, though liable to
mutations of very long periods, they return again exactly to what they
originally were, oscillating between very narrow limits; but he found a
zone of instability between the orbit of Mars, and twice the mean
distance of the earth from the sun,[1] or between 1·5 and 2·00;
therefore the position and form of the orbits of such of the telescopic
planets as revolve within that zone will be subject to unlimited
variations. But the orbits of those more remote from the sun than Flora,
or beyond 2·20, will be stable, so that their excentricities and
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