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
I was some years since assured by Mr. Maclure of Philadelphia, that
whenever any doubt or hesitation betrayed itself with respect to
its fertilizing agency, it was only necessary to sprinkle a small
quantity in a meadow, to satisfy the most sceptical; and that this
was usually done in the form of letters or characters, which in
a short time became so much more luxuriant than the surrounding
grass, as to be visible at a considerable distance. It is, I
understand, chiefly applied to grass lands as a _top-dressing_; and
the American farmers[112] explain its operation upon its solubility
in water, and its consequent absorption by the roots of the grass.
Davy, in examining the ashes of sainfoin, clover, and rye-grass,
which had grown in soils manured by gypsum, found considerable
quantities of that substance; and he thinks it probable that it
was intimately connected with their woody fibre. He attempts to
explain the reason why the application of gypsum is not generally
efficacious, by supposing that most of the cultivated soils may
already contain it in sufficient quantities for the use of the
grasses. I strongly suspect, however, that it will be hereafter
discovered to depend upon the nature of the soil in its hygrometric
relations. From the facts already recorded, it would appear that
it never answers near the sea, nor in wet lands. In consequence of
its solubility, it is enabled to penetrate and pervade the whole
vegetable structure; and the experiments of Davy have proved its
presence in the ashes of plants exposed to its operation, and have
rendered it probable that it enters into union with their woody
fibre, by which the density of their textures will be increased,
and consequently the evaporation from their leaves diminished; I
am from such considerations induced to think that gypsum does not
act by effecting any chemical change in the soil, but solely by
diminishing the plants evaporation. This idea seems to be borne out
by the evidence furnished by the different circumstances attending
the operation of this manure: we find, for example, that succulent
vegetables, planted on dry soils, are those which are principally
benefited by its application, and that the various grasses so
manured retain their verdure, even in the dryest season and on
the most arid lands; at the same time, we find that these crops,
especially clover, acquire a proportionate increase in the density
of their fibres, that is to say, that they become much more rank
and stubborn, and often to such a degree does this take place,
that in America, where its effects are best understood, sheep
not uncommonly refuse to feed upon them. Upon the same principle
we find that, under circumstances or in situations where the
evaporation of a plant is provided for by a constant supply of
moisture, the effects of gypsum cease to be apparent.
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