The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
It should also be added that, even independently of actual collisions,
there is, and must be, loss of energy in the system from other causes.
There are no absolutely rigid bodies known in nature, for the hardest
mineral or the toughest steel must yield to some extent when large
forces are applied to it, and as the bodies in the system are not mere
points or particles of inconsiderable dimensions, they will experience
stresses something like those to which our earth is subjected in that
action of the moon and sun which produces the tides. In consequence of
the influences of each body on the rest, there will be certain relative
changes in the parts of each body; there will be, as it were, tidal
movements in their liquid parts and even in their solid substance. These
tides will produce friction, and this will produce heat. This heat will
be radiated from the system, but the heat radiated corresponds to a
certain amount of energy; the energy is therefore lost to the system, so
that even without actual collisions we still find that energy must be
gradually lost to the system.
Thus we have been conducted to an important conclusion, which may be
stated in the following way. Let there be any system of bodies, subject
to their mutual attractions, and sufficiently isolated from the
disturbing influence of all bodies which do not belong to the system,
then the original energy with which that system is started must be
undergoing a continual decline. It must at least decline until such a
condition of the system has been reached that collisions are no longer
possible and that tidal influences have ceased. These conditions might
be fulfilled if all the bodies of the system coalesced into a single
mass.
As illustrations of the systems we are now considering, we may take the
sun and planets as a whole. A spiral nebula is a system in the present
sense, while perhaps the grandest illustration of all is provided by the
Milky Way.
It will be noted that we may have a system which is isolated so far as
our present argument is concerned, even while it forms a part of another
system of a higher order of magnitude. For instance, Saturn with his
rings and satellites is sufficiently isolated from the rest of the solar
system and the rest of the universe, to enable us to trace the
consequences of the gradual decline of energy in his attendant system.
The solar system in which Saturn appears merely as a unit, is itself
sufficiently isolated from the stars in the Milky Way to permit us to
study the decline of energy in the solar system, without considering the
action of those stars.
Public-domain text, read in full here on John Shaqi.
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