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
And such changes do naturally come over the soil. The oak, after
thriving for long generations on a particular spot, gradually sickens;
its entire race dies out,—and other races succeed it. The operation
of natural causes has gradually removed from the soil that which
favoured the oak, and has introduced or given the predominance to those
substances which favour the beech or the pine.
In the hands of the farmer the land grows sick of this crop,—it becomes
tired of that. These facts are generally indications of a change in
the chemical constitution of the soil. This alteration may proceed
slowly and for many years, and the same crops may still grow upon it
for a succession of rotations. At length the change is too great for
the plant to bear; it sickens, yields an unhealthy crop, and becomes
ultimately extinct.
The plants we raise for food have similar likes and dislikes with those
that are naturally produced. On some kinds of food they thrive,—fed
with others, they sicken or die. The soil must therefore be prepared
for their special growth.
In an artificial rotation of crops, we only follow nature. One crop
extracts from the soil a certain quantity of all the inorganic
constituents of plants; but some of these in much larger proportions
than others. A second crop carries off in preference a larger quantity
of those substances which the former had left; and thus it is clearly
seen, both why an abundant manuring may so alter the constitution of
the soil, as to enable it to grow almost any crop; and why, at the same
time, this soil may in succession yield more abundant crops and in
greater number, if the kinds of plant sown and reaped be so varied as
to extract from the soil, one after the other, the several different
substances which the manure we have originally added is known to
contain.
The management and tilling of the soil, in fact, is a branch of
practical chemistry, which, like the art of dyeing or of lead smelting,
may advance to a certain degree of perfection, without the aid of pure
science; but which can only have its processes explained, and be led on
to shorter,—more simple,—more economical,—and more perfect processes,
by the aid of scientific principles.
CHAPTER VIII.
Of the Improvement of the Soil—Mechanical and Chemical
Methods—Draining—Subsoiling—Ploughing, and Mixing
of Soils—Use of Lime, Marl, and Shell-sand—Manures
—Vegetable, Animal, and Mineral Manures.
The soil is possessed of certain existing and obvious qualities, and
of certain other dormant capabilities; how are these qualities to be
improved,—these dormant capabilities to be awakened?
Public-domain text, read in full here on John Shaqi.
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