The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
We can also express the total energy of the solar system in a different
manner. We shall consider what must be the velocity of the sun, so that
the energy that it will possess, in virtue of that velocity, shall be
equal to the energy which could be produced by the combustion of 8,300
globes of coal of the same weight. This calculation is very much
simplified by making use of a principle which we have already stated and
applied in Chapter V. We have shown that if a piece of coal be animated
with a velocity of five miles a second, the energy it possesses in
virtue of that motion is equal to the energy produced by the coal in the
act of combustion. If a body were moving at the rate of, let us say, 100
miles a second—its speed being then twenty times as great as the
particular speed just mentioned—its energy, which depends on the square
of the velocity, would be 400 times as much as would be produced by the
burning of a piece of coal equal to it in weight. We can easily
calculate that if the sun were moving at a speed of 460 miles a second,
it would possess, in virtue of its motion, as much energy as would be
generated by the contraction of the primæval nebula from infinity down
to a globe of the density of platinum.
It is thus easy to form a supposition as to how the nebula constituting
our solar system may have come into being; most probably it originated
in this way. Let us suppose that two masses, either dark or bright,
either hot or of the temperature of space, or the temperature of frozen
air, were moving with speeds of 460 miles a second. No doubt the
velocities we are here postulating are very high velocities, but they
are not unprecedentedly high. We know of stars which at this present
moment move quite as fast, so that there is nothing unreasonable in our
supposition so far as the velocities are concerned. Let us suppose that
each of these bodies had a mass which is half that of our present solar
system. If these two bodies dashed into collision, when moving from
opposite directions, the effect of the blow would be to transform the
energy into heat. That heat would be so great that it would be
sufficient not alone to render these globes red-hot and white-hot, but
even to fuse them—nay, further, to drive them into vapour, even to a
vapour which might expand to an enormously great distance. In other
words, it is quite conceivable that a collision of two such masses as we
have here supposed might be adequate to the formation of a nebula such
as that one which in the lapse of indefinite ages has shaped itself into
the solar system.
Before the collision, which resulted in the formation of the nebula,
each of these bodies, or rather their centres of gravity, would be
moving in what may be regarded for the moment as straight lines, and a
plane through those two straight lines will be a plane which for ever
afterwards will stand in important relation to the system. It will be,
in fact, that principal plane of which we have so often spoken.
Public-domain text, read in full here on John Shaqi.
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