The Botanic Garden, a Poem in Two Parts. Part 1: the Economy of VegetationDarwin, Erasmus
History
The Botanic Garden, a Poem in Two Parts. Part 1: the Economy of Vegetation
Darwin, Erasmus
Natural history; Plants -- Poetry; Portland Vase
A cubic inch of water thus cooled down to 32 deg. mixed with an equal
quantity of boiling water at 212 deg. will cool it to the middle number
between these two, or to 122. But a cubic inch of ice whose sensible
cold also is but 32, mixed with an equal quantity of boiling water, will
cool it six times as much as the cubic inch of cold water
above-mentioned, as the ice not only gains its share of the sensible or
gravitating heat of the boiling water but attracts to itself also and
combines with the quantity of latent heat which it had lost at the time
of its congelation.
So boiling water will acquire but 212 deg. of heat under the common pressure
of the atmosphere, but the steam raised from it by its expansion or by
its solution in the atmosphere combines with and carries away a
prodigious quantity of heat which it again parts with on its
condensation; as is seen in common distillation where the large quantity
of water in the worm-tub is so soon heated. Hence the evaporation of
ether on a thermometer soon sinks the mercury below freezing, and hence
a warmth of the air in winter frequently succeeds a shower.
When the matter of heat or calorique is set at liberty from its
combinations, as by inflammation, it passes into the surrounding bodies,
which possess different capacities of acquiring their share of the loose
or sensible heat; thus a pint measure of cold water at 48 deg. mixed with a
pint of boiling water at 212 deg. will cool it to the degree between these
two numbers, or to 154 deg., but it requires two pint measures of
quicksilver at 48 deg. of heat to cool one pint of water as above. These and
other curious experiments are adduced by Dr. Black to evince the
existance of combined or latent heat in bodies, as has been explained by
some of his pupils, and well illustrated by Dr. Crawford. The world has
long been in expectation of an account of his discoveries on this
subject by the celebrated author himself.
As this doctrine of elementary heat in its fluid and combined state is
not yet universally received, I shall here add two arguments in support
of it drawn from different sources, viz. from the heat given out or
absorbed by the mechanical condensation or expansion of the air, and
perhaps of other bodies, and from the analogy of the various phenomena
of heat with those of electricity.
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