The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
In the beginning of the evolutionary history the sun was a nebula, which
we have supposed to extend in every direction to an indefinitely great
distance. The system has resulted from the contraction of that nebula,
and the energy liberated in that contraction has supplied the sun’s
radiation. We calculate (_see_ Appendix) the energy that would be given
out in the contraction of a nebula whose materials were originally at
infinity, and which ultimately coalesced to form a cold, solid globe of
the density of platinum, and as heavy as the sun. There is no object in
attempting to express this quantity of energy in foot-pounds—the figures
would convey no distinct impression—we shall employ the coal-unit
explained in Chapter VI. We imagine a globe of coal the weight of the
sun; then, if that globe of coal were adequately supplied with oxygen,
it would, on combustion, give out a certain amount of heat, which is a
convenient unit for our measurements. It is demonstrated that the
quantity of energy given out by the contraction of the nebula from
infinity, to this globe of the density of platinum, would be about equal
to the quantity of energy which would be produced by the combustion of
8,300 globes of coal as heavy as the sun, an adequate contribution of
oxygen being supposed to be supplied. This expresses the original
endowment of energy in the solar system, or rather a major limit to that
endowment; it shows that the solar system can never have developed more
energy by contraction than that which could be produced by the
combustion of 8,300 globes of coal as heavy as the sun. We may mention
that of this great endowment of energy an amount which is rather less
than half (3,400) has been already expended, so that rather more than
half of the sun’s career as a radiant globe may yet have to be run.
Public-domain text, read in full here on John Shaqi.
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