The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
We must push our argument further still. We have ascertained that the
primæval sun could not have been a dense solid body like a ball of
metal. It must have been more nearly represented by a ball of gas. There
was a time when that collection of matter which now constitutes the sun
was so big that a balloon of equal size, filled at ordinary pressure
with the lightest of known gases, would contain within it a heavier
weight than the sun. At this early period the sun must have been as
light as an equal volume of hydrogen. The reasoning which has conducted
us to this point remains still unimpaired. From that early period we may
therefore look back to periods earlier still. We see that the sun must
have been ever larger and larger, for the same quantity of material must
have been ever more and more diffused. There was a time when the mean
density of the sun must have been far less than that of the gas in any
balloon.
We must not pause to consider intermediate stages. We shall look back at
once to an excessively early period when the sun—or perhaps we ought
rather to say the matter which in a more condensed form now constitutes
the sun—was expanded throughout the volume of a globe whose radius was
as great as the present distance from the sun to the earth. Have we not
here truly an astonishing result, deduced as a necessary consequence
from the fundamental laws of heat?
[Illustration: Fig. 20.—THE SOLAR CORONA (January 1st, 1899).
(_Photographed during Eclipse by Professor W. H. Pickering._)]
I need hardly say that the sun at that early date did not at all
resemble the glorious orb to which we owe our very existence. The
primæval sun must have been a totally different object, as we can easily
imagine if we try to think that the sun’s materials then filled a volume
twelve million times as great as they occupy at present. Instead of
comparing such an object with the gases in our ordinary atmosphere, it
should rather be likened to the residue left in an exhausted receiver
after the resources of chemistry have been taxed to make as near an
approach as possible to a perfect vacuum.
We can give a familiar illustration of gas in a state of extreme
tenuity. Look at the beautiful incandescent light with which in these
days our buildings are illuminated. How brilliantly those little globes
shine! The globe has to be most carefully sealed against the outside
air. If there were the smallest opportunity for access, the air from
outside would rush in and the lamp would be destroyed. In the
preparation of such a lamp elaborate precautions have to be taken to
secure that the exhaustion of the air from the little globe shall be as
nearly perfect as possible. Of course it is impossible to remove all the
air. No known processes can produce a perfect vacuum. Some traces of gas
would remain after the air-pump had been applied even for hours.
Public-domain text, read in full here on John Shaqi.
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