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
It is interesting to note the infallible tendency of energy to revert
to its original form of axial energy, or energy of rotation, by means of
the air machine. All Nature bears witness to this tendency, and although
the path of energy through the maze of terrestrial transformation often
appears tortuous and uncertain, its final destination is always sure.
The secondary operations are thus interlinked into one great whole by
their association in the terrestrial energy cycle. Many of these
secondary operations are of short duration; others extend over long
periods of time. Energy, in some cases, appears to slumber, as in the
coal seams of the earth, until an appropriate stimulus is applied, when
it enters into active operation once more. The cyclical operations are
thus long or short according to the duration of their constituent
secondary energy processes. But the balance of Nature is ever preserved.
Axial energy, transformed by the working of one cyclical process, is
being as continuously returned by the simultaneous operation of others.
PART III
TERRESTRIAL CONDITIONS
33. _Gaseous Expansion_
Before proceeding to the general description of the atmospheric machine
(§ 10), it is desirable to consider one or two features of gaseous
reaction which have a somewhat important bearing on its working. Let it
be assumed that a mass of gaseous material is confined within the lower
portion of a narrow tube ABCD (Fig. 8) assumed to be thermally
non-conducting; the upper portion of the tube is in free communication
with the atmosphere. The gas within the tube is assumed to be isolated
from the atmosphere by a movable piston EF, free to move vertically in
the tube, and for the purpose of illustration, assumed also frictionless
and weightless. With these assumptions, the pressure on the confined gas
will simply be that due to the atmosphere. If heat energy be now
applied to the gas, its temperature will rise and expansion will ensue.
This expansion will be carried out at constant atmospheric pressure; the
gaseous material, as it expands, must lift with it the whole of the
superimposed atmospheric column against the downward attractive force of
the earth's gravitation on that column. Work is thus done by the
expanding gas, and in consequence of this work done, a definite quantity
of atmospheric material gains energy of position or potential energy
relative to the earth's surface. At the same time, the rise of
temperature of the gas will indicate an accession of heat energy to its
mass. These familiar phenomena of expansion under constant pressure
serve to illustrate the important fact that, when heat energy is applied
to a gaseous mass, it really manifests itself therein in two aspects,
namely, heat energy and work energy. The increment of heat energy is
indicated by the increase in temperature, the increment of work energy
by the increase in pressure. In the example just quoted, however, there
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