Philosophical transactions, Vol. L. Part I. For the year 1757.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.Various
History
Philosophical transactions, Vol. L. Part I. For the year 1757.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.
Various
Science -- Periodicals
But since the aforesaid quantity, from whence the motion of the earth’s
equinox is derived, as well by this gentleman, as by Sir Isaac Newton,
expresses truly the annual regress of the equinoctial points of the
ring (and not of the hollow figure formed by the said matter, which
is greater, in the ratio of 5 to 4) it seems, at least, as reasonable
to suppose, that the said quantity, to obtain from thence the true
regress of the equinoctial points of the earth, ought to be diminished
in the former of the two ratios above specified, as that it should be
diminished in the latter. But, indeed, both these ways are defective,
even supposing the momenta to have been truly computed; the ratio,
that ought to be used here, being that of the momenta of the ring and
earth about the proper axe of rotation of the two figures, standing
at right-angles to the plane of the ring and of the equator. Now this
ratio, by a very easy computation, is found to be as 230²-229² to ⅖ of
230²; whence the quantity sought comes out = (3co-s. 23° 29´/4 rad.)
× (⅟366¼) × (230²-229²)/230² × 360° = 21´´ 6´´´: which is the same that
we before found it to be, and the double of what this author makes it.
What has been said hitherto, relates to that part of the motion
only, arising from the force of the sun. It will be but justice to
observe here, that the effect of the moon, and the inequalities
depending on the position of her nodes, are truly assigned by both
the gentlemen above-named; the ratio of the diameters of the earth,
and the density of the moon being so assumed, as to give the maxima of
those inequalities, such as the observations require: in consequence
whereof, and from the law of the increase and decrease (which is
rightly determined by theory, tho’ the absolute quantity is not) a true
solution, in every other circumstance, is obtained.
The freedom, with which I have expressed myself, and the liberty I have
here taken, to animadvert on the works of men, who, in many places,
have given incontestible proofs of skill and genius, may, I fear, stand
in need of some apology. ’Tis possible I may be thought too peremptory.
Indeed, I might have delivered my sentiments with more caution and
address: but, had not I imagined myself quite clear in what has been
advanced, from a multitude of concurrent reasons, I should have thought
it too great a presumption to have said any thing at all here, on this
subject. The great regard I have for this Society, of which I have the
honour to be a member, will, I hope, be considered as the motive for my
having attempted to rectify some oversights, that have occurred in the
works of this learned body.
LIV. _Remarks upon the Heat of the Air in_ July 1757. _in an Extract
of a Letter from_ John Huxham, _M.D. F.R.S. to_ William Watson, _M.D.
F.R.S. dated at_ Plymouth _19th of that Month. With additional Remarks
by Dr._ Watson.
[Read Dec. 22, 1757.]
Public-domain text, read in full here on John Shaqi.
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