The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
It is equally true that when the nebula is contracting, and when the
distance between every two particles is lessening, the nebula must be
giving out energy, because the total energy in the contracted state is
less than it was in the expanded state. This energy is equivalent to
heat. We need not here pause to consider by what actual process the heat
is manifested; it suffices to say that the heat must, by one of the
general laws of Nature, be produced in some form.
We are now able to make a numerical estimate. We shall suppose that the
earth, or rather the materials which make the earth, existed originally
as a large nebula distributed through illimitable space. The
calculations show that the quantity of heat, generated by the
condensation of those materials from their nebulous form into the
condition which the earth now has, was enormously great. We need not
express this quantity of heat in ordinary units. The unit we shall take
is one more suited to the other dimensions involved. Let us suppose a
globe of water as heavy as the earth. This globe would have to be five
or six times as large as the earth. Next let us realise the quantity of
heat that would be required to raise that globe of water from freezing
point to boiling point. It can be proved that the heat, or its
equivalent, which would be generated merely by the contraction of the
nebula to form the earth, would be ninety times as great as the amount
of heat which would suffice to raise a mass of water equal in weight to
the earth from freezing point to boiling point.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account