The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
To investigate whether the solar heat can be attributed to chemical
combination, we shall assume for the moment that the sun is composed of
those particular materials which would produce the utmost quantity of
heat for a given weight; in other words, that the sun is formed of
hydrogen and oxygen in quantities having the same ratio as that in which
they should be united to form water. The quantity of heat generated by
the union of known weights of oxygen and hydrogen has been ascertained,
by experiments in the laboratory, to exceed that which can be generated
by corresponding weights of any other materials. We can calculate how
much of the sun’s mass, if thus constituted, would have to enter into
combination every hour in order to generate as much heat as the hourly
radiation of the sun. We need not here perform the actual calculation,
but merely state the result, which is a very remarkable one. It shows
that the heat arising from the supposed chemical action would not
suffice to sustain the radiation of the sun at its present rate for more
than 3,000 years. Thirty centuries is a long time, no doubt, yet still
we must remember that it is no more than a part even of the period known
to human history. If, indeed, it had been by combustion that the sun’s
heat was produced, then from the beginning of the sun’s career as a
luminous object to its final extinction and death could not be longer
than 3,000 years, if we assumed that its radiation was to be uniformly
that which it now dispenses.
But it may be said that we are dealing only with elements known to us
and with which terrestrial chemists are familiar, and it may be urged
that the sun possibly contains materials whose chemical union produces
heat in much greater abundance than do the elements with which alone we
are acquainted. But this argument cannot be sustained. One of the most
important discoveries of the last century, the discovery which perhaps
more than any other has tended to place the nebular theory in an
impregnable position, is that which tells us that the elements of which
the sun is composed are the same as the elements of which our earth is
made. We shall have to refer to this in detail in a later chapter. We
now only make this passing reference to it in order to dismiss the
notion that there can be unknown substances in the sun whose heat of
combustion would be sufficiently great to offer an explanation of the
extraordinary abundance of solar radiation.
Public-domain text, read in full here on John Shaqi.
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