The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
Professor Joly has made an estimate of the quantity of salt daily added
to the sea by all the rivers of the globe. He has also made an estimate
of the total quantity of salt which is at present contained in the sea.
He has thus the means of forming an estimate of the number of years
necessary for the sea to have become converted from its primæval
freshness to its present saltness. His result is not a little
astonishing. The saltness of the sea could not be accounted for unless
the rivers had been running into the sea for at least a hundred million
years. This period is five times as long as the total period during
which the sun could have been shining if the Helmholtzian view were
correct.
Of course, there are many elements of uncertainty in such a calculation.
We have assumed that the total flow of the rivers is practically
constant, and that our estimate fairly represents the average salinity
of river water. We have also made a large assumption in supposing that
we have accurately estimated the total volume of salt in the oceans. But
taken in conjunction with the geological evidence already referred to,
taken in conjunction with the immense periods of time that have been
required for the evolution of life on the globe by the process of
natural selection, the conclusion arrived at is inevitable. It seems
impossible to doubt that the sun must have been shining and that our
solar system must have existed in practically the same form as it is at
present for periods enormously greater than would have been possible if
the heat of the sun had been sustained by the solar contraction only.
The difficulty here indicated has been not unjustly considered the most
serious difficulty with which the development of modern physical and
astronomical science has been confronted. The time during which the sun
must have lasted, according to the received explanation of the source of
its heat and the time during which the sun has actually lasted, as shown
by the facts of geology, present a wide discrepancy. Science demands
that some reconciliation must be effected, yet how is that to be
accomplished? There is only one possible solution of the problem. It is
obvious that there must have been some vast reserve of heat in the sun
in comparison with which the quantity of heat yielded by the contraction
may be deemed insignificant. Until this new source of solar energy had
been discovered, our knowledge of the physics of the solar system lay
under a reproach, which it was the bounden duty of men of science to
endeavour to remove.
During the last few years lines of research carried on in various
directions have, in a most unexpected manner, thrown much light on the
origin of the sun’s heat, and, indeed, we may now say that the great
difficulty which has for so long troubled us no longer exists in a
serious form.
Public-domain text, read in full here on John Shaqi.
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