Science in Short ChaptersWilliams, W. Mattieu (William Mattieu)
Science
Science in Short Chapters
Williams, W. Mattieu (William Mattieu)
Science
The most remarkable part of Dr. Wollaston’s paper is the _reductio ad
absurdum_ by which he seeks to finally demonstrate the finite extent of
our atmosphere. He maintains, as I do, that if the elasticity of our
atmosphere is unlimited, its extension must be commensurate with the
universe, that every orb in space will, by gravitation, gather around
itself an atmosphere proportionate to its gravitating power, and that,
by taking the known quantity of the earth’s atmosphere as our unit, we
may calculate the amount of atmosphere possessed by any heavenly body
of which the mass is known. On this basis Dr. Wollaston calculates
the atmosphere of the sun, and concludes that its extent will be so
great as to visibly affect the apparent motions of Mercury and Venus,
when their declination makes its nearest approach to that of the sun.
No such disturbance being actually observable, he concludes that such
an atmosphere as he has calculated cannot exist. In like manner he
calculates the atmosphere of Jupiter, and finds it to be so great, that
its refraction would be sufficient “to render the fourth satellite
visible to us when behind the centre of the planet, and consequently to
make it appear on both (or all) sides at the same time.”
On examining these calculations, I have discovered the very curious
error above referred to. As this is a matter of figures that cannot
be abridged, I must refer the reader to the original calculations. I
will here merely state that Wollaston’s method of calculating the solar
gravitation atmosphere and that of Jupiter and the moon leads to the
monstrous conclusion that, in ascending from the surface of the given
orb, we always have the same limited amount of atmospheric matter above
as that with which we started, although we are continually leaving a
portion of it below.
Public-domain text, read in full here on John Shaqi.
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