(111.) It is not alone by the direct fall of bodies that the
gravitation of the earth is manifested. The curvilinear motion of
bodies projected in directions different from the perpendicular, is
a combination of the effects of the uniform velocity which has been
given to the projectile by the impulse which it has received, and the
accelerated velocity which it receives from the earth’s attraction.
Suppose a body placed at any point P, _fig. 21._, above the
surface of the earth, and let P C be the direction of the earth’s
centre. If the body were allowed to move without receiving any impulse,
it would descend to the earth in the direction P A, with an
accelerated motion. But suppose that at the moment of its departure
from P, it receives an impulse in the direction P B, which would
carry it to B in the time the body would fall from P to A, then, by
the composition of motion, the body must at the end of that time be
found in the line B D, parallel to P A. If the motion in
the direction of P A were uniform, the body P would in this case
move in the straight line from P to D. But this is not the case. The
velocity of the body in the direction P A is at first so small as
to produce very little deflection of its motion from the line P B.
As the velocity, however, increases, this deflection increases, so that
it moves from P to D in a curve, which is convex, towards P B.
The greater the velocity of the projectile in the direction P A,
the greater sweep the curve will take. Thus it will successively take
the forms P D, P E, P F, &c., and that velocity can be
computed, which (setting aside the resistance of the air) would cause
the projectile to go completely round the earth, and return to the
point P from which it departed. In this case, the body P would continue
to revolve round the earth like the moon. Hence it is obvious, that the
phenomenon of the revolution of the moon round the earth, is nothing
more than the combined effects of the earth’s attraction, and the
impulse which it received when launched into space by the hand of its
Creator.
(112.) This is a great step in the analysis of the phenomenon of
gravitation. We have thus reduced to the same class two effects
apparently very dissimilar, the rectilinear descent of a heavy body,
and the nearly circular revolution of the moon round the earth. Hence
we are conducted to a generalisation still more extensive.
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