Popular lectures on scientific subjects : $b Second series, with an autobiography of the authorHelmholtz, Hermann von
Science
Popular lectures on scientific subjects : $b Second series, with an autobiography of the author
Helmholtz, Hermann von
Science; Universities and colleges -- Germany
On earth the processes of combustion are the most abundant source of
heat. Does the sun’s heat originate in a process of this kind? To this
question we can reply with a complete and decided negative, for we
now know that the sun contains the terrestrial elements with which we
are acquainted. Let us select from among them the two, which, for the
smallest mass, produce the greatest amount of heat when they combine;
let us assume that the sun consists of hydrogen and oxygen, mixed in
the proportion in which they would unite to form water. The mass of
the sun is known, and also the quantity of heat produced by the union
of known weights of oxygen and hydrogen. Calculation shows that under
the above supposition, the heat resulting from their combustion would
be sufficient to keep up the radiation of heat from the sun for 3,021
years. That, it is true, is a long time, but even profane history
teaches that the sun has lighted and warmed us for 3,000 years, and
geology puts it beyond doubt that this period must be extended to
millions of years.
Known chemical forces are thus so completely inadequate, even on the
most favourable assumption, to explain the production of heat which
takes place in the sun, that we must quite drop this hypothesis.
We must seek for forces of far greater magnitude, and these we can
only find in cosmical attraction. We have already seen that the
comparatively small masses of shooting-stars and meteorites can produce
extraordinarily large amounts of heat when their cosmical velocities
are arrested by our atmosphere. Now the force which has produced these
great velocities is gravitation. We know of this force as one acting
on the surface of our planet when it appears as terrestrial gravity.
We know that a weight _raised from the earth_ can drive our clocks,
and that in like manner the gravity of the water rushing down from the
mountains works our mills.
If a weight falls from a height and strikes the ground its mass loses,
indeed, the visible motion which it had as a whole--in fact, however,
this motion is not lost; it is transferred to the smallest elementary
particles of the mass, and this invisible vibration of the molecules is
the motion of heat. Visible motion is transformed by impact, into the
motion of heat.
That which holds in this respect for gravity, holds also for
gravitation. A heavy mass, of whatever kind, which is suspended in
space separated from another heavy mass, represents a force capable
of work. For both masses attract each other, and, if unrestrained by
centrifugal force, they move towards each other under the influence of
this attraction; this takes place with ever-increasing velocity; and
if this velocity is finally destroyed, whether this be suddenly, by
collision, or gradually, by the friction of movable parts, it develops
the corresponding quantity of the motion of heat, the amount of which
can be calculated from the equivalence, previously established, between
heat and mechanical work.
Public-domain text, read in full here on John Shaqi.
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