Six Lectures on Light: Delivered In The United States In 1872-1873Tyndall, John
Science
Six Lectures on Light: Delivered In The United States In 1872-1873
Tyndall, John
Light
Let us now mount our Nicol prisms, and cross them as we crossed the
tourmaline. Introducing our film of gypsum between them, you notice
that in one particular position the film has no power whatever over
the field of view. But, when the film is turned a little way round,
the light passes. We have now to understand the mechanism by which
this is effected.
First, then, we have a prism which receives the light from the
electric lamp, and which is called the _polarizer_. Then we have the
plate of gypsum (supposed to be placed at S, fig. 36), and then the
prism in front, which is called the _analyzer_. On its emergence from
the first prism, the light is polarized; and, in the particular case
now before us, its vibrations are executed in a horizontal plane. We
have to examine what occurs when the two directions of vibration in
the interposed gypsum are oblique to the horizon. Draw a rectangular
cross (A B, C D, fig. 37) to represent these two directions. Draw a
line (_a_ _b_) to represent the amplitude of the horizontal vibration
on the emergence of the light from the first Nicol. Let fall from each
end of this line two perpendiculars (_a_ _c_, _a_ _f_, _b_ _d_, _b_
_e_) on the two arms of the cross; then the distances (_c_ _d_, _e_
_f_) between the feet of these perpendiculars represent the amplitudes
of two rectangular vibrations, which are the _components_ of the first
single vibration. Thus the polarized ray, when it enters the gypsum,
is resolved into its two equivalents, which vibrate at right angles to
each other.
[Illustration; Fig. 37.]
In one of these two rectangular directions the ether within the gypsum
is more sluggish than in the other; and, as a consequence, the waves
that follow this direction are more retarded than the others. In both
cases the undulations are shortened when they enter the gypsum, but
in the one case they are more shortened than in the other. You can
readily imagine that in this way the one system of waves may get half
a wave-length, or indeed any number of half wavelengths, in advance of
the other. The possibility of interference here at once flashes upon
the mind. A little consideration, however, will render it evident
that, as long as the vibrations are executed at right angles to each
other, they cannot quench each other, no matter what the retardation
may be. This brings us at once to the part played by the analyzer. Its
sole function is to recompound the two vibrations emergent from the
gypsum. It reduces them to a single plane, where, if one of them be
retarded by the proper amount, extinction will occur.
Public-domain text, read in full here on John Shaqi.
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