The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
We represent by arrows in Fig. 36 the directions in which A, B, and C
are moving at the moment. We choose any point O in the plane, and for
simplicity we have so drawn the figure that A, B, and C are forces
tending to turn round O in the same direction. The velocity of a body
multiplied into its mass is termed the _momentum_ of the body. Draw the
perpendicular from O to the direction in which the body A is moving,
then the product of this perpendicular and the momentum of A is called
the _moment of momentum_ of A around O. In like manner we form the
moment of momentum of B and C, and if we add them together we obtain the
total moment of momentum of the system.
We can now give expression to a great discovery which mathematicians
have made. No matter how complicated may be the movements of A, B, and
C; no matter to what extent these particles approximate or how widely
they separate; no matter what changes may occur in their velocities, or
even what actual collision may take place, the sum of the moments of
momentum must remain for ever unaltered. This most important principle
in dynamics is known as the conservation of moment of momentum.
Though I have only mentioned three particles, yet the same principle
will be true for any number. If it should happen that any of them are
turning round O in the opposite direction, then their moments of
momentum are to be taken as negative. In this case we add the moments
tending in one direction together; and then subtract all the opposite
moments. The remainder is the quantity which remains constant.
[Illustration: Fig. 36.—TO ILLUSTRATE MOMENT OF MOMENTUM.]
We may state this principle in a somewhat different manner as follows:
Let us consider a multitude of particles in a plane; let them be
severally started in any directions in the plane, and then be abandoned
to their mutual attractions, it being understood that there are no
forces produced by bodies external to the system; if we then choose any
point in the plane, and measure the areas described round that point by
the several moving bodies in one second, and if we multiply each of,
those areas by the mass of the corresponding body, then, if all the
bodies are moving in the same direction round the point, the sum of the
quantities so obtained is constant. It will be the same a hundred or a
thousand years hence as it is at the present moment, or as it was a
hundred or a thousand years ago. If any of the particles had been
turning round the point in the opposite direction, then the products
belonging to such particles are to be subtracted from the others instead
of added.
Public-domain text, read in full here on John Shaqi.
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