On a Dynamical Top, for exhibiting the phenomena of the motion of a system of invariable form about a fixed point, with some suggestions as to the Earth's motionMaxwell, James Clerk
Science
On a Dynamical Top, for exhibiting the phenomena of the motion of a system of invariable form about a fixed point, with some suggestions as to the Earth's motion
Maxwell, James Clerk
Force and energy; Motion
It is easy to understand the motion of a body revolving about a fixed
axle. Every point in the body describes a circle about the axis, and
returns to its original position after each complete revolution. But if
the axle itself be in motion, the paths of the different points of the
body will no longer be circular or re-entrant. Even the velocity of
rotation about the axis requires a careful definition, and the
proposition that, in all motion about a fixed point, there is always
one line of particles forming an instantaneous axis, is usually given
in the form of a very repulsive mass of calculation. Most of these
difficulties may be got rid of by devoting a little attention to the
mechanics and geometry of the problem before entering on the discussion
of the equations.
Mr Hayward, in his paper already referred to, has made great use of the
mechanical conception of Angular Momentum.
Definition 1 The Angular Momentum of a particle about an axis is
measured by the product of the mass of the particle, its velocity
resolved in the normal plane, and the perpendicular from the axis on
the direction of motion.
* The angular momentum of any system about an axis is the algebraical
sum of the angular momenta of its parts.
As the _rate of change_ of the _linear momentum_ of a particle measures
the _moving force_ which acts on it, so the _rate of change_ of
_angular momentum_ measures the _moment_ of that force about an axis.
All actions between the parts of a system, being pairs of equal and
opposite forces, produce equal and opposite changes in the angular
momentum of those parts. Hence the whole angular momentum of the system
is not affected by these actions and re-actions.
* When a system of invariable form revolves about an axis, the angular
velocity of every part is the same, and the angular momentum about the
axis is the product of the _angular velocity_ and the _moment of
inertia_ about that axis.
* It is only in particular cases, however, that the _whole_ angular
momentum can be estimated in this way. In general, the axis of angular
momentum differs from the axis of rotation, so that there will be a
residual angular momentum about an axis perpendicular to that of
rotation, unless that axis has one of three positions, called the
principal axes of the body.
By referring everything to these three axes, the theory is greatly
simplified. The moment of inertia about one of these axes is greater
than that about any other axis through the same point, and that about
one of the others is a minimum. These two are at right angles, and the
third axis is perpendicular to their plane, and is called the mean
axis.
* Let $A$, $B$, $C$ be the moments of inertia about the principal axes
through the centre of gravity, taken in order of magnitude, and let
$\omega_1$ $\omega_2$ $\omega_3$ be the angular velocities about them,
then the angular momenta will be $A\omega_1$, $B\omega_2$, and
$C\omega_3$.
Public-domain text, read in full here on John Shaqi.
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