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
With monochromatic light the rings would be simply bright and
black--the bright rings occurring at those thicknesses of the spar
which cause the rays to conspire; the black rings at those thicknesses
which cause them to quench each other. Turning the analyzer 90° round,
we obtain the complementary phenomena. The black cross gives place to
a bright one, and every dark ring is supplanted also by a bright one
(fig. 46). Here, as elsewhere, the different lengths of the
light-waves give rise to iris-colours when white light is employed.
[Illustration: Fig. 46.]
[Illustration: Fig. 47.]
Besides the _regular_ crystals which produce double refraction in no
direction, and the _uniaxal_ crystals which produce it in all
directions but one, Brewster discovered that in a large class of
crystals there are _two_ directions in which double refraction does
not take place. These are called _biaxal_ crystals. When plates of
these crystals, suitably cut, are placed between the polarizer and
analyzer, the axes (A A', fig. 47) are seen surrounded, not by
circles, but by curves of another order and of a perfectly definite
mathematical character. Each band, as proved experimentally by
Herschel, forms a _lemniscata_; but the experimental proof was here,
as in numberless other cases, preceded by the deduction which showed
that, according to the undulatory theory, the bands must possess this
special character.
§ 10. _Power of the Wave Theory_.
I have taken this somewhat wide range over polarization itself, and
over the phenomena exhibited by crystals in polarized light, in order
to give you some notion of the firmness and completeness of the theory
which grasps them all. Starting from the single assumption of
transverse undulations, we first of all determine the wave-lengths,
and find that on them all the phenomena of colour are dependent. The
wavelengths may be determined in many independent ways. Newton
virtually determined them when he measured the periods of his Fits:
the length of a fit, in fact, is that of a quarter of an undulation.
The wave-lengths may be determined by diffraction at the edges of a
slit (as in the Appendix to these Lectures); they may be deduced from
the interference fringes produced by reflection; from the fringes
produced by refraction; also by lines drawn with a diamond upon glass
at measured distances asunder. And when the length determined by these
independent methods are compared together, the strictest agreement is
found to exist between them.
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