An Introduction to the History of ScienceLibby, Walter
History
An Introduction to the History of Science
Libby, Walter
Science -- History
Under this heading we have to consider a single illustration--the
prediction, and the discovery, in 1846, of the planet Neptune. This
event roused great enthusiasm among scientists as well as in the popular
mind, afforded proof of the reliability of the Newtonian hypothesis, and
demonstrated the precision to which the calculation of celestial motions
had attained. Scientific law appeared not merely as a formulation and
explanation of observed phenomena but as a means for the discovery of
new truths. "Would it not be admirable," wrote Valz to Arago in 1835,
"to arrive thus at a knowledge of the existence of a body which cannot
be perceived?"
The prediction and discovery of Neptune, to which many minds
contributed, and which has been described with a show of justice as a
movement of the times, arose from the previous discovery of the planet
Uranus by Sir William Herschel in 1781. After that event Bode suggested
that it was possible other astronomers had observed Uranus before,
without recognizing it as a planet. By a study of the star catalogues
this conjecture was soon verified. It was found that Flamsteed had made,
in 1690, the first observation of the heavenly body now called Uranus.
Ultimately it was shown that there were at least seventeen similar
observations prior to 1781.
It might naturally be supposed that these so-called ancient observations
would lead to a ready determination of the planet's orbit, mass, mean
distance, longitude with reference to the sun, etc. The contrary,
however, seemed to be the case. When Alexis Bouvard, the associate of
Laplace, prepared in 1821 tables of Uranus, Jupiter, and Saturn on the
principles of the _Mécanique Céleste_, he was unable to fix an orbit for
Uranus which would harmonize with the data of ancient and modern
observations, that is, those antecedent and subsequent to Herschel's
discovery in 1781. If he computed an orbit from the two sets of data
combined, the requirements of the earlier observations were fairly well
met, but the later observations were not represented with sufficient
precision. If on the other hand only the modern data were taken into
account, tables could be constructed meeting all the observations
subsequent to 1781, but failing to satisfy those prior to that date. A
consistent result could be obtained only by sacrificing the modern or
the ancient observations. "I have thought it preferable," says Bouvard,
"to abide by the second [alternative], as being that which combines the
greater number of probabilities in favor of the truth, and I leave it to
the future to make known whether the difficulty of reconciling the two
systems result from the inaccuracy of ancient observations, or whether
it depend upon some extraneous and unknown influence, which has acted on
the planet." It was not till three years after the death of Alexis
Bouvard that the extraneous influence, of which he thus gave in 1821
some indication, became fully known.
Public-domain text, read in full here on John Shaqi.
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