The Energy System of Matter: A Deduction from Terrestrial Energy PhenomenaWeir, James, active 1883-1912
Science
The Energy System of Matter: A Deduction from Terrestrial Energy Phenomena
Weir, James, active 1883-1912
Force and energy
The energy phenomena illustrated by the experimental devices above are
to be observed, in their aspects of greatest perfection, in the natural
world. In the earth, united to its encircling atmosphere by the
invisible bond of gravitation, we find the prototype of the hypothetical
system just described. Its uniformity of rotation is an established fact
of centuries, and over its spheroidal surface we have, corresponding to
the motion of our illustrative spherical masses, the movement of
enormous quantities of atmospheric air in the general directions from
equatorial to polar regions and vice versa. This circulatory movement,
and the internal energy reactions which it involves, have been already
fully dealt with (§ 88); we have now to consider it in a somewhat more
comprehensive fashion, in the light of the pendulum systems described
above. As already explained (§ 13), the operation of mechanical energy
is not confined to solid and liquid masses only, but may likewise be
manifested by the movements of gaseous masses. The terrestrial
atmospheric machine provides an outstanding example. In its working
conditions, and in the general nature of the energy operations involved,
the terrestrial atmospheric machine is very clearly represented by the
rotating pendulum system (§ 42). The analogy is still closer in the case
of the hypothetical system just described. The actual terrestrial energy
machine differs from both only in that the energy processes, which they
illustrate by the movements of solid material, are carried out in the
course of its working by the motion of gaseous masses. It is obvious,
however, that this in no way affects the inherent nature of the energy
processes themselves. They are carried out quite as completely and
efficiently--in fact, more completely and more efficiently--by the
motions of gaseous as by the motions of solid material.
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