The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
To the sublime conceptions of the theologian succeeded the desire for
exact knowledge characteristic of the man of science. Whatever its
ultimate cause might have been, the proximate cause of the rainbow
was physical, and the aim of science was to account for the bow on
physical principles. Progress toward this consummation was very slow.
Slowly the ancients mastered the principles of reflection. Still more
slowly were the laws of refraction dug from the quarries in which
Nature had imbedded them. I use this language because the laws were
incorporate in Nature before they were discovered by man. Until the
time of Alhazan, an Arabian mathematician, who lived at the beginning
of the Twelfth Century, the views entertained regarding refraction
were utterly vague and incorrect. After Alhazan came Roger Bacon and
Vitellio, who made and recorded many observations and measurements on
the subject of refraction. To them succeeded Kepler, who, taking the
results tabulated by his predecessors, applied his amazing industry
to extract from them their meaning--that is to say, to discover
the physical principles which lay at their root. In this attempt
he was less successful than in his astronomical labors. In 1604,
Kepler published his _Supplement to Vitellio_, in which he virtually
acknowledged his defeat by enunciating an approximate rule, instead
of an all-satisfying natural law. The discovery of such a law, which
constitutes one of the chief corner-stones of optical science, was
made by Willebrod Snell, about 1621.
A ray of light may, for our purposes, be presented to the mind as a
luminous straight line. Let such a ray be supposed to fall vertically
upon a perfectly calm water-surface. The incidence, as it is called,
is then perpendicular, and the ray goes through the water without
deviation to the right or left. In other words, the ray in the air
and the ray in the water form one continuous straight line. But the
least deviation from the perpendicular causes the ray to be broken,
or “refracted,” at the point of incidence. What, then, is the law
of refraction discovered by Snell? It is this, that no matter how
the angle of incidence and with it the angle of refraction may vary,
the relative magnitude of two lines, dependent on these angles,
and called their sines, remains, for the same medium, perfectly
unchanged. Measure, in other words, for various angles, each of these
two lines with a scale, and divide the length of the longer one by
that of the shorter; then, however the lines individually vary in
length, the quotient yielded by this division remains absolutely the
same. It is, in fact, what is called “the index of refraction” of the
medium.
Public-domain text, read in full here on John Shaqi.
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