Science for the School and Family, Part I. Natural PhilosophyHooker, Worthington
Science
Science for the School and Family, Part I. Natural Philosophy
Hooker, Worthington
Physics; Science
331. =Why the Above Exception to Expansion by Heat Exists.=--That
we may see the reasons in part for the grand exception to the
general law of expansion by heat which I have illustrated, let us
see what would be some of the results if the exception did not
exist. In that case the process of freezing would be as follows:
The water would communicate its heat from the surface to the air,
as before described, and there would be a constant downward current
of the cooled water. When any portion of the water became cooled
by the air down to 32°, it would become ice, and would sink to the
bottom. And after the process of freezing had once begun, there
would be a continual accumulation of ice at the bottom so long as
the air remained cold enough to cool the water with which it comes
in contact down to 32°.
The result may be stated in the general thus: Freezing would not
begin so quickly as it now does; but when once begun it would prove
very destructive. It would not begin as soon, because the whole
of any body of water must be cooled down to just this side of 32°
before it could begin. This would not take long where the water
is shallow, but it would where it is deep. All shallow bodies of
water, then, would be frozen up quite early in the winter; and as
water is a poor conductor, and thawing must go from above downward,
some of them would not be thawed out again fully till quite into
the next summer, if even then. And where the water is quite deep
ice would at length begin to form, and when formed it would be
exceedingly slow in thawing. In some cases it would never be thawed
with such a body of non-conducting water to guard it against the
warmth above. It is easy to see that the heat of spring and summer
would not thaw out any thing like the quantity of ice that it now
does. The reign of ice and snow on our earth would therefore be
vastly more extensive than now, and what is worse, it would be
extended more and more every year. Under such circumstances there
would be great destruction of both animal and vegetable life. I
will mention, however, but a single item, as it would occupy too
much space to go into this subject with any fullness. In the water
under the ice, which is always above 39°, except that which is
close to the ice when freezing is going on, there is a vast amount
of busy life which would be destroyed if ice were formed at the
bottom, chilling all the water above.
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