Science in Short ChaptersWilliams, W. Mattieu (William Mattieu)
Science
Science in Short Chapters
Williams, W. Mattieu (William Mattieu)
Science
Regarding the properties of our atmosphere only in the light
of experimental data, irrespective of imaginary molecules, and
their supposed gyrations or oscillations, we see at once that an
inter-planetary or inter-stellar vacuum must act like a Sprengel
pump upon our atmosphere, upon the atmosphere of other planets, and
upon those of the sun and the stars, and would continue such action
until an equilibrium between the repulsive energy of the gas and the
gravitation of the solid orbs had been established. Atmospheric matter
would thus be universally diffused, with special accumulations around
solid orbs, varying in quantity with their respective gravitating
energy. Such a universal atmosphere would accelerate orbital motion,
and this acceleration would vary with the surface of bodies. Its action
being thus exactly opposed to that of radiant repulsion, it must, at a
certain density, exactly neutralize it. That it does this is evident
from the obedience of all the elements of the solar system to the
calculated action of gravitation; and thus Mr. Crookes’s researches
not only confirm the idea of universal atmospheric diffusion, but they
afford a means by which we may ultimately measure the actual density of
the universal atmosphere. If, as I have endeavored to show in my essay
on “The Fuel of the Sun,” the initial radiant energy of every star
depends upon its mass, and its consequent condensation of atmospheric
matter, the density of inter-planetary atmosphere sufficient to
neutralize the radiant mechanical energy of our sun may be the same
as is demanded to perform the same function for all the stars of the
universe, and all their attendant worlds, comets, and meteors.
Public-domain text, read in full here on John Shaqi.
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