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
The perfection of the polarization in a direction perpendicular to the
illuminating beam may be also illustrated by the following experiment,
which has been executed with many vapours. A Nicol prism large enough
to embrace the entire beam of the electric lamp was placed between the
lamp and the experimental tube. Sending the beam polarized by the
Nicol through the tube, I placed myself in front of it, the eyes being
on a level with its axis, my assistant occupying a similar position
behind the tube. The short diagonal of the large Nicol was in the
first instance vertical, the plane of vibration of the emergent beam
being therefore also vertical. As the light continued to act, a superb
blue cloud visible to both my assistant and myself was slowly formed.
But this cloud, so deep and rich when looked at from the positions
mentioned, utterly disappeared when looked at vertically downwards,
or vertically upwards. Reflection from the cloud was not possible in
these directions. When the large Nicol was slowly turned round its
axis, the eye of the observer being on the level of the beam, and the
line of vision perpendicular to it, entire extinction of the light
emitted horizontally occurred when the longer diagonal of the large
Nicol was vertical. But a vivid blue cloud was seen when looked at
downwards or upwards. This truly fine experiment, which I should
certainly have made without suggestion, was, as a matter of fact,
first definitely suggested by a remark addressed to me in a letter by
Professor Stokes.
All the phenomena of colour and of polarization observable in the case
of skylight are manifested by those actinic clouds; and they exhibit
additional phenomena which it would be neither convenient to pursue,
nor perhaps possible to detect, in the actual firmament. They enable
us, for example, to follow the polarization from its first appearance
on the barely visible blue to its final extinction in the coarser
cloud. These changes, as far as it is now necessary to refer to them,
may be thus summed up:--
1. The actinic cloud, as long as it continues blue, discharges
polarized light in all directions, but the direction of maximum
polarization, like that of skylight, is at right angles to the
direction of the illuminating beam.
2. As long as the cloud remains distinctly blue, the light discharged
from it at right angles to the illuminating beam is _perfectly_
polarized. It may be utterly quenched by a Nicol prism, the cloud from
which it issues being caused to disappear. Any deviation from the
perpendicular enables a portion of the light to get through the prism.
3. The direction of vibration of the polarized light is at right
angles to the illuminating beam. Hence a plate of tourmaline, with its
axis parallel to the beam, stops the light, and with the axis
perpendicular to the beam transmits the light.
Public-domain text, read in full here on John Shaqi.
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