The Forms of Water in Clouds and Rivers, Ice and GlaciersTyndall, John
Science
The Forms of Water in Clouds and Rivers, Ice and Glaciers
Tyndall, John
Clouds; Glaciers; Ice; Rivers; Water
307. We now take a common finger-glass and put into it a little
pounded ice and salt. On this we place the flask, and then build
round it the freezing mixture. The liquid column retreats down the
tube, proving the contraction of the liquid by cold. We allow the
shrinking to continue for some minutes, noticing that the downward
retreat of the liquid becomes gradually slower, and that it finally
ceases altogether.
308. Keep your eye upon the liquid column; it remains quiescent for
a fraction of a minute, and then moves once more. But its motion is
now _upwards_ instead of downwards. _The freezing mixture now acts
exactly like the flame._
309. It would not be difficult to pass a thermometer through the cork
into the flask, and it would tell us the exact temperature at which
the liquid ceased to contract and began to expand. At that moment we
should find the temperature of the liquid a shade over 39° Fahr.
310. At this temperature, then, water attains _its maximum density_.
311. Seven degrees below this temperature, or at 32° Fahr., the
liquid begins to turn into solid crystals of ice, which you know
swims upon water because it is bulkier for a given weight. In fact,
this halt of the approaching molecules at the temperature of 39°,
is but the preparation for the subsequent act of crystallisation,
in which the expansion by cold culminates. Up to the point of
solidification the increase of volume is slow and gradual; while in
the act of solidification it is sudden, and of overwhelming strength.
312. By this force of expansion the Florentine Academicians long
ago burst a sphere of copper nearly three quarters of an inch in
thickness. By the same force the celebrated astronomer Huyghens burst
in 1667 iron cannons a finger breadth thick. Such experiments have
been frequently made since. Major Williams during a severe Quebec
winter filled a mortar with water, and closed it by driving into
its muzzle a plug of wood. Exposed to a temperature 50° Fahr. below
the freezing point of water, the metal resisted the strain, but the
plug gave way, being projected to a distance of 400 feet. At Warsaw
howitzer shells have been thus exploded; and you and I have shivered
thick bombshells to fragments, by placing them for half an hour in a
freezing mixture.
313. The theory of the shafts and pits referred to at the beginning
of this section is this: The water at the surface of the shaft is
warmed by the sun, say to a temperature of 39° Fahr. The water at
the bottom, in contact with the ice, must be at 32° or near it. The
heavier water is therefore at the top; it will descend to the bottom,
melt the ice there, and thus deepen the shaft.
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