The Life of Sir Humphry Davy, Bart. LL.D., Volume 1 (of 2)Paris, John Ayrton
Science
The Life of Sir Humphry Davy, Bart. LL.D., Volume 1 (of 2)
Paris, John Ayrton
Chemists -- England -- Biography; Davy, Humphry, Sir, 1778-1829
[107] The history of his native county would have furnished
him with a parallel instance of the intelligence and design
which Nature displays in connecting the wants and necessities
of the different parts of creation, with the power and means
of supplying them. In a primitive country like Cornwall, the
siliceous soil necessarily requires much moisture, and we may
perceive that the cause which occasions, at the same time
supplies this want; for the rocks elevated above the surface,
solicit a tribute from every passing cloud; while in alluvial
and flat districts, where the soil is rich, deep, and retentive
of moisture, the clouds float undisturbed over the plains, and
the country frequently enjoys that uninterrupted series of dry
weather which is so necessary to its fertility. Linnæus observes,
that the plants which chiefly grow upon the summit of mountains,
are rarely found in any other situation, except in marshes,
because the clouds arrested in their progress by such elevations,
keep the air in a state of perpetual moisture.
If water in its elastic and fluid states be essentially necessary
to the economy of vegetation, so even in its solid form, it is not
without its uses. Snow and ice are bad conductors of heat; and at
a period when the severity of the winter threatens the extinction
of vegetable life, Nature kindly throws her snowy mantle over the
surface; while in early spring the solution of the snow becomes the
first nourishment of the plant; at the same time, the expansion of
water in the act of congelation, and the subsequent contraction of
its bulk during a thaw, tend to pulverise the soil, to separate
its parts from each other, and, by making it more permeable to the
influence of the air, to prepare it for the offices it is destined
to perform.
He next proceeds to consider the action of the atmosphere on
plants, and to connect it with a general view of the progress
of vegetation. He commences with examining its relations to
germination.
"If a healthy seed be moistened and exposed to air at a temperature
not below 45°, it soon germinates; it shoots forth a _plume_ which
rises upwards, and a _radicle_ which descends.
"If the air be confined, it is found that, in the process of
germination, the oxygen, or a part of it, is absorbed. The azote
remains unaltered; no carbonic acid is taken away from the air; on
the contrary, some is added." Upon this point, critics have been
disposed to break a lance with Sir Humphry.
The doctrine, let it be observed, is at variance with the numerous
experiments made on this subject by Scheele, Cruickshank, and De
Saussure; the results of which agree in proving, that if seeds be
confined and made to germinate in a given portion of air, not a
_part_ only, but the _whole_ of the oxygen is consumed; and that
its place is supplied, not merely by _some_, but by an _equal bulk_
of carbonic acid.
Public-domain text, read in full here on John Shaqi.
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