The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
Let A and S be simply released from initial positions of absolute rest.
In these circumstances, the two points will start off towards each
other. The time that must elapse before the two bodies collide will
depend upon circumstances. The greater the initial distance between the
two balls, their sizes being the same, the longer must be the interval
before they come together. The relation between the distance separating
the bodies and the time that must elapse before they meet may be
illustrated in this way. Suppose that two balls, both starting from rest
at a certain distance, should take a year to come together by their
mutual attraction, then we know that if the distance of the two balls
had been four times as great eight years would have to elapse before the
two balls collided. If the distances were nine times as great then
twenty-seven years would elapse before the balls collided, and generally
the squares of the times would increase as the cubes of the distances.
In such statements we are supposing that the radii of the balls are
inconsiderable in comparison with the distances apart from which they
are started. The time occupied in the journey must also generally depend
on the masses of the two bodies, or, to speak more precisely, on the sum
of the masses of the two bodies. If the two balls each weighed five
hundred tons, then they would take precisely the same time to rush
together as would two balls of one ton and nine hundred and ninety-nine
tons respectively, provided the distances between the centres of the two
balls had been the same in each case. If the united masses of the two
bodies amounted to four thousand tons, then they would meet in half the
time that would have been required if their united masses were one
thousand tons, it being understood that in each case they started with
the same initial distance between the centres.
Instead of simply releasing the two bodies A and S so that neither of
them shall have any impulse tending to make it swerve from the line
directly joining them, let us now suppose that we give one of the
bodies. A, a slight push sideways. The question will be somewhat simpler
if we think of S as very massive, while A is relatively small. If, for
instance, S be as heavy as a cannon-ball, while A is no heavier than a
grain of shot, then we may consider that S remains practically at rest
during the movement. The small pull which A is able to give will produce
no more than an inappreciable effect on S. If the two bodies come
together, A will practically do all the moving.
[Illustration: Fig. 46.—THE PLANE OF A PLANET’S ORBIT.]
Public-domain text, read in full here on John Shaqi.
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