Fragments of Science: A Series of Detached Essays, Addresses, and Reviews. V. 1-2Tyndall, John
Science
Fragments of Science: A Series of Detached Essays, Addresses, and Reviews. V. 1-2
Tyndall, John
Chemistry; Physics; Science
As regards the polarisation of skylight, the greatest stumbling-block
has hitherto been, that, in accordance with the law of Brewster, which
makes the index of refraction the tangent of the polarising angle, the
reflection which produces perfect polarisation would require to be
made in air upon air; and indeed this led many of our most eminent
men, Brewster himself among the number, to entertain the idea of
aerial molecular reflection. [Footnote: 'The cause of the
polarisation is evidently a reflection of the sun's light upon
something. The question is on what? Were the angle of maximum
polarisation 76°, we should look to water or ice as the reflecting
body, however inconceivable the existence in a cloudless atmosphere
and a hot summer's day of unevaporated molecules (particles?) of
water. But though we were once of this opinion, careful observation
has satisfied us that 90°, or thereabouts, is the correct angle, and
that therefore whatever be the body on which the light has been
reflected, if polarised by a single reflection, the polarising angle
must be 45°, and the index of refraction, which is the tangent of that
angle, unity; in other words, the reflection would require to be made
in air upon air!' (Sir John Herschel, 'Meteorology,' par. 233.)
Any particles, if small enough, will produce both the colour and the
polarisation of the sky. But is the existence of small
water-particles on a hot summer's day in the higher regions of our
atmosphere inconceivable? It is to be remembered that the oxygen and
nitrogen of the air behave as a vacuum to radiant heat, the
exceedingly attenuated vapour of the higher atmosphere being therefore
in practical contact with the cold of space.]
I have, however, operated upon substances of widely different
refractive indices, and therefore of very different polarising angles
as ordinarily defined, but the polarisation of the beam, by the
incipient cloud, has thus far proved itself to be absolutely
independent of the polarising angle. The law of Brewster does not
apply to matter in this condition, and it rests with the undulatory
theory to explain why. Whenever the precipitated particles are
sufficiently fine, no matter what the substance forming the particles
may be, the direction of maximum polarisation is at right angles to
the illuminating beam, the polarising angle for matter in this
condition being invariably 45°.
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