A Manual Of Photography
Forfatter: Robert Hunt
År: 1853
Forlag: John Joseph Griffin & Co.
Sted: London
Udgave: 3
Sider: 370
UDK: 77.02 Hun
Third Edition, Enlarged
Illustrated by Numerous Engrabings
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148 SCIENTIFIC INVESTIGATIONS ON PHOTOGRAPHE.
„à of decomposing the iodide of silver in a longer or shorter
time as they have that of producing the affinity for mercury on
the bromo-iodide of silver: with the difference, that on the
former compound the separate actions of the several! rave. con-
tinue each other, and that on the second compound these
separate actions destroy each other. We can understand that
in the first case, all the rays are capable of operating the same
decomposition ; and that in the second, the affinity for mercury
when imparted by one ray is destroyed by another. U>>sw°u^
explain the various phenomena of the formation of the two
different deposits, and also the anomaly of the continuation ot
the action by the red, orange or yellow rays, according to M Ed.
Becquerel's discoveries on the iodide of silver ; and of the de-
struction of that action by the same rays according to M.
Claudet’s observations on the bromo-iodide of silver.
The red, orange, and yellow rays, when acting on an unaffected
surface, are considerably less capable than the most refran-
Sble rays of imparting the affinity for inercuria vapour on
both the iodide and bromo-iodide of silver ; and they destroy
that affinity when it has been produced on the
silver by the photogenic rays. It follows from this fact, that
when the red, orange, or yellow rays are more abundant in the
light than the most refrangible rays, the photogenic effect is
retarded in proportion to the excess of these antagonistic rays.
This happens when there exist in the atmosphere some vapours
which absorb the most refrangible rays. In these circumstances
the light appears rather yellow ; but it is very difficult to judge
by the eye of the exact colour of the light, and of the proportion
of photogenic rays existing in the atmosphere at any given
moment. , ,. r
The vapours of the atmosphere which render the light yellow,
act as any other medium intercepting the blue rays, and those
which have the same degree of refrangibility.
If we cover an engraving one-half with light yellow glass, and
place it before a camera obscura, in order to represent the
whole on a daguerreotype plate we shall find that during the
time which has been necessary to obtain the image of the halt
not covered, not the slightest effect has been produced on the
half covered with the yellow glass.
Now, if we cover one-half with deep blue glass, and the other
with the same light yellow glass, the engraving will be seen very
distinctly through the yellow glass, and not at all through the
blue. In representing the whole, as before on the daguerreotype
plate, the half which was clearly seen by the eye has produced
no effect; and in the other, which could not be seen, is as fui y