The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
There is perhaps no greater question in the study of Nature than that
which enquires how the sun’s heat is sustained so that the radiation is
still dispensed with unstinted liberality. If we are asked how the sun
can be fed so as to sustain this expenditure, we have to explain that
the sun is not really fed. If, then, it receives no adequate supplies of
energy from without, we have to admit that the sun must be getting
exhausted.
I ought, indeed, to anticipate objection by at once making the admission
that the sun does receive some small supply of energy from the meteors
which are perennially drawn into it. The quantity of energy they yield
is, however, insignificant in comparison with the solar expenditure of
heat. We may return to this subject at a later period, and it need not
now receive further attention.
We must deliberately face the fact that the energy of the sun is
becoming exhausted. But the rate of exhaustion is so slow that it
affords no prospect of inconvenience to humanity; it does not excite
alarm. We grant that we are not able to observe by instrumental means
any perceptible diminution of solar energy. Still, as we know that
energy is being steadily dissipated from the sun, and that energy cannot
be created from nothing, it is certain the decline is in progress. But
the reserve of energy which the sun possesses, and which can be
ultimately rendered available to sustain the radiation, is so enormous
in comparison with the annual expenditure of energy, that myriads of
centuries will have to elapse before there is any appreciable alteration
in the effectiveness of the sun.
Let me illustrate the point by likening the sun to a grain warehouse, in
which 2,500 tons of wheat can be accommodated. Let us suppose that the
warehouse was quite full at the beginning, and that the wheat was to be
gradually abstracted, but only at the rate of one grain each day. Let us
further suppose that no more wheat is to be added to that already in the
warehouse, and let us assume that the wheat thus stored away experiences
no deterioration and no loss whatever except by the removal of one grain
per diem. It is easy to see that very many centuries would have to
elapse before the grain in that warehouse had decreased to any
appreciable extent.
With a consumption at the rate of a single grain a day a ton of corn
would last about four thousand years, and 2,500 tons of corn would
accordingly last about ten million years. It follows, therefore, that if
the grain in that store were consumed at the rate of only one grain per
day the warehouse would not be emptied for ten million years.
[Illustration: Fig. 15.—I. SPECTRUM OF THE SUN.
II. SPECTRUM OF ARCTURUS.
(_Professor H. C. Lord._)]
Public-domain text, read in full here on John Shaqi.
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