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
masses would tend to move radially outwards on the arms as they move
towards the regions of highest velocity. Let this radial movement be
carried out against the action of four radial springs S{1}, S{2},
S{3}, S{4}, as shown (Fig. 11). In virtue of the radial movement of
the masses, these springs will be compressed and energy stored in them
in the form of energy of strain or cohesion (§ 15). The radial movement
implies also that the masses will be elevated from the surface of the
imaginary sphere over which they are assumed to move. The elevation from
this surface will be greatest in the regions of high velocity in the
neighbourhood of H and L, and least at A and B. As the masses move,
therefore, from H and L towards the axis AB, they will also move inwards
on the pendulum arms, relieving the springs, so that the energy stored
in them is free to be returned to the system in its original form of
energy of rotation. Every movement of the masses from the central axis
outwards against the springs is thus made at the expense of the original
energy of motion, and every movement inwards provokes a corresponding
return of that energy to the system. Every movement also against the
springs forms part of a reversible operation. The sum total of the
energy which works in these reversible operations is always less than
the complete energy of the rotatory system, and the latter is always
stable (§ 25), with respect to its energy properties. Let it now be
assumed that the complete system as described is possessed of a precise
and limited amount of energy of rotation, and that with the pendulum
masses in an intermediate position as shown (Fig. 11) it is rotating
with uniform angular velocity. The condition of the rotatory system
might now be described as that of equilibrium. A definite amount of its
original rotatory energy is now stored in the central spring and also in
the radial springs. If now, without alteration in the intrinsic rotatory
energy of the system, the pendulum masses were to execute a vibratory or
pendulum motion about the position of equilibrium so that they move
alternately to and from the central axis, then as they move inwards
towards that axis the energy stored in the springs would be returned to
the system in the original form of energy of rotation. This inward
motion would, accordingly, produce acceleration. But, in the outward
movement from the position of equilibrium, retardation would ensue on
account of energy of motion being withdrawn from the system and stored
in the springs.
[Illustration: FIG. 11]
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