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
In the natural world, we find processes of the same general nature in
constant operation. When any mass of material is elevated from the
surface of a rotating planetary body against the gravitative attraction,
it thereby gains energy of position (§ 20). This energy, on the body's
return to the surface in the course of its cycle, reappears in the form
of energy of motion. Now the material mass, in rising from the planetary
surface, is not, in reality, separated from the planet. The atmosphere
of the planet forms an integral portion of its material, partakes of its
rotatory motion, and is bound to the solid core by the mutual
gravitative forces. Any mass, then, on the solid surface of a planet is,
in reality, in the planetary interior, and the rising of such a mass
from that surface does not imply any actual separative process, but
simply the radial movement, or displacement of a portion of the
planetary material from the central axis. If the energy expended in the
upraisal of the mass is derived at the expense of the inherent rotatory
energy of the planet, as it would be if the latter were a strictly
conservative energy system, then the raising of this portion of
planetary material from the surface would have a retarding effect on the
planetary motion of rotation. But if, on the other hand, the energy of
such a mass as it fell towards the planetary surface were converted once
more into its original form of energy of axial motion, exactly
equivalent in amount to its energy of position, it is evident that the
process would be productive of an accelerating effect on the planetary
motion of rotation, which would in magnitude exactly balance the
previous retardation. In such a process it is evident that energy
neither enters nor leaves the planet. It simply works in an energy
machine embodied in planetary material. This point will be more fully
illustrated later. The reader will readily see the resemblance of a
system of this nature to that which has already been illustrated by the
rotating pendulum.
In the meantime, it may be pointed out that matter displaced from the
planetary surface need not necessarily be matter in the solid form. All
the operations mentioned above could be quite readily--in fact, more
readily--carried out by the movements of gaseous material, which is
admirably adapted for every kind of rising, falling, or flowing motion
relative to the planetary surface (§ 13).
27. _Some Phenomena of Transmission Processes--Transmission of Heat
Energy by Solid Material_
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