The principles of science : $b a treatise on logic and scientific methodJevons, William Stanley
Philosophy
The principles of science : $b a treatise on logic and scientific method
Jevons, William Stanley
Logic; Science -- Methodology
absolute standard of time, then all other bodies must be subject to the
same arbitrary fits and starts, otherwise there would be discrepancy
disclosing the irregularities. Just as in comparing together a number
of chronometers, we should soon detect bad ones by their going
irregularly, as compared with the others, so in nature we detect
disturbed movement by its discrepancy from that of other bodies which
we believe to be undisturbed, and which agree nearly among themselves.
But inasmuch as the measure of motion involves time, and the measure
of time involves motion, there must be ultimately an assumption. We
may define equal times, as times during which a moving body under the
influence of no force describes equal spaces;[214] but all we can
say in support of this definition is, that it leads us into no known
difficulties, and that to the best of our experience one freely moving
body gives the same results as any other.
[214] Rankine, *Philosophical Magazine*, Feb. 1867, vol. xxxiii.
p. 91.
When we inquire where the freely moving body is, no perfectly
satisfactory answer can be given. Practically the rotating globe is
sufficiently accurate, and Thomson and Tait say: “Equal times are
times during which the earth turns through equal angles.”[215] No long
time has passed since astronomers thought it impossible to detect any
inequality in its movement. Poisson was supposed to have proved that a
change in the length of the sidereal day amounting to one ten-millionth
part in 2,500 years was incompatible with an ancient eclipse recorded
by the Chaldæans, and similar calculations were made by Laplace. But
it is now known that these calculations were somewhat in error, and
that the dissipation of energy arising out of the friction of tidal
waves, and the radiation of the heat into space, has slightly decreased
the rapidity of the earth’s rotatory motion. The sidereal day is now
longer by one part in 2,700,000, than it was in 720 B.C. Even before
this discovery, it was known that invariability of rotation depended
upon the perfect maintenance of the earth’s internal heat, which is
requisite in order that the earth’s dimensions shall be unaltered. Now
the earth being superior in temperature to empty space, must cool more
or less rapidly, so that it cannot furnish an absolute measure of time.
Similar objections could be raised to all other rotating bodies within
our cognisance.
[215] *Treatise on Natural Philosophy*, vol. i. p. 179.
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