The Earth's BeginningBall, Robert S. (Robert Stawell)
Science
The Earth's Beginning
Ball, Robert S. (Robert Stawell)
Krakatoa (Indonesia); Nebular hypothesis
But among all possible planes there is one of special significance in
its relation to the system. It is called the “principal plane,” and it
is characterised by the fact that the sum (with due attention to sign)
of the areas described each second by the feet of the perpendiculars,
multiplied into the masses of the corresponding particle, is greater
than the like magnitude for any other plane, and is thus a maximum. For
all planes parallel to this principal plane, the result will be, of
course, the same; it is the direction of the plane and not its absolute
situation that is material. We thus see that while this remarkable
quantity is constant in any plane, for all time, yet the actual value of
that constant depends upon the aspect of the plane; for some planes it
is zero, for others the constant has intermediate values, and there is
one plane for which the constant is a maximum. This is the principal
plane, and a knowledge of it is of vital importance in endeavouring to
understand the nebular theory. Nor are the principles under
consideration limited only to a system consisting of sun and planets;
they apply, with suitable modifications, to many other celestial systems
as well.
The instructive character of this dynamical principle will be seen when
we deduce its consequences. The term “moment of momentum” of a particle,
with reference to a certain point in a plane, expresses double the
product of the rate at which the area is described by the foot of the
perpendicular to this plane, multiplied by the mass of the particle. The
moment of momentum of the system, with reference to the principal plane,
is a maximum in comparison with all other planes; that moment of
momentum retains precisely the same value throughout all time, from the
first instant the system was started onwards. And it retains this value,
no matter what changes or disturbances may happen in the system,
provided only that the influence of external forces is withheld. Subject
to this condition, the transformations of the system may be any
whatever. The several bodies may be forced into wide changes of their
orbits, so that there may even be collisions among them; yet,
notwithstanding those collisions, and notwithstanding the violent
alterations which may be thus produced in the movements of the bodies,
the moment of momentum will not alter. No matter what tides may be
produced, even if those tides be so great as to produce disruption in
the masses and force the orbits to change their character radically, yet
the moment of momentum will be conserved without alteration.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account