The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
It has already been stated that a layer of water less than the twentieth
of an inch in thickness suffices to stop and destroy all waves of
radiant heat emanating from an obscure source. The longer waves of the
obscure heat cannot get through water, and I find that all transparent
compounds which contain _hydrogen_ are peculiarly hostile to the longer
undulations. It is, I think, the presence of this element in the
humours of the eye which prevents the extra red rays of the solar
spectrum from reaching the retina. It is interesting to observe that
while bisulphide of carbon, chloride of phosphorus, and other liquids
which contain no hydrogen, permit a large portion of the rays emanating
from an iron or copper ball, at a heat below redness, to pass through
them with facility, the same thickness of substances equally
transparent, but which contain hydrogen, such as ether, alcohol, water,
or the vitreous humour of the eye of an ox, completely intercepts these
obscure rays. The same is true of solid bodies; a very slight thickness
of those which contain hydrogen offers an impassable barrier to all rays
emanating from a non-luminous source.[A] But the heat thus intercepted
is by no means lost; its _radiant form_ merely is destroyed. Its waves
are shivered upon the particles of the body, but they impart warmth to
it, while the heat which retains its radiant form contributes in no way
to the warmth of the body through which it passes.
[Sidenote: FINAL COLOUR OF ICE AND WATER BLUE.]
Water then absorbs all the extra red rays of the sun, and if the layer
be thick enough it invades the red rays themselves. Thus the greater the
distance the solar beams travel through pure water the more are they
deprived of those components which lie at the red end of the spectrum.
The consequence is, that the light finally transmitted by the water, and
which gives to it its colour, is _blue_.
[Sidenote: EXPERIMENT.]
I find the following mode of examining the colour of water both
satisfactory and convenient:--A tin tube, fifteen feet long and three
inches in diameter, has its two ends stopped securely by pieces of
colourless plate glass. It is placed in a horizontal position, and pure
water is poured into it through a small lateral pipe, until the liquid
reaches half way up the glasses at the ends; the tube then holds a
semi-cylinder of water and a semi-cylinder of air. A white plate, or a
sheet of white paper, well illuminated, is then placed at a little
distance from one end of the tube, and is looked at through the tube.
Two semicircular spaces are then seen, one by the light which has passed
through the air, the other by the light which has passed through the
water; and their proximity furnishes a means of comparison, which is
absolutely necessary in experiments of this kind. It is always found
that, while the former semicircle remains white, the latter one is
vividly coloured.[B]
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