Elements of agricultural chemistry and geologyJohnston, Jas. F. W. (James Finlay Weir)
Science
Elements of agricultural chemistry and geology
Johnston, Jas. F. W. (James Finlay Weir)
Agricultural chemistry
There are none so little skilled in regard to the capabilities of the
soil, as not to be aware that some lands naturally produce abundant
herbage or rich crops, while others refuse to yield a nourishing
pasture, and are deaf to the often repeated solicitations of the
diligent husbandman. There exists, therefore, a universally understood
connection between the kind of soil and the kind of plants that
naturally grow upon it. It is interesting to observe how close this
relation in many cases is.
1. The sands of the sea-shore, and the margins of salt-lakes, are
distinguished by their peculiar tribes of salt-loving plants;—the
drifted sands more remote from the beach produce their own long waving
coarser grass,—while further inland again, other vegetable races appear.
2. Peaty soils laid down to grass, or existing as natural meadows,
produce one woolly soft grass almost exclusively (the _Holcus
lanatus_); when limed, again, these same soils become propitious to
green crops and produce much straw, but refuse to fill the ear.
3. On the margins of water-courses, in which silica abounds, the
mare’s-tail (_Equisetum_) springs up in abundance; while, if the stream
contain much carbonate of lime, the water-cress appears and lines its
sides, and the bottom of its shallow bed, sometimes for many miles from
its source.
4. The Cornish heath (_Erica vagans_) shews itself only above the
serpentine rocks; the red clover and the vetch delight in the presence
of gypsum; and white clover, of alkaline matter in the soil.
5. Then, again, plants seem to alternate with each other on the same
soil. Burn down a forest of pines in Sweden, and one of birch takes
its place _for a while_. The pines after a time again spring up and
ultimately supersede the birch. The same takes place naturally. On the
shores of the Rhine are seen ancient forests of oak from two to four
centuries old,—gradually giving place to a natural growth of beech; and
others where the pine is succeeding to both. In the Palatinate, the
ancient oak woods are followed by natural pines; and in the Jura, the
Tyrol, and Bohemia, the pine alternates with the beech.
These and other similar differences depend upon the chemical
constitution of the soil. The slug may live well, and therefore infest
a field almost deficient in lime; the common land snail will abound at
the roots of the hedges only where lime is plentiful, and can easily
be obtained for the construction of its shell. So it is with plants.
Each grows spontaneously where its wants can be most fully and most
easily supplied. If they cannot move from place to place like the
living animal, yet their seeds can lie dormant, until either the hand
of man or the operation of natural causes produces such a change in the
constitution of the soil as to fit it for ministering to their most
important wants.
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