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
Oxide of Iron, }
Oxide of manganese, } 0 ½ trace.
Silica, 81 73½ 80
Sulphuric acid, 1 2 1½
Phosphoric acid, 5 3 ¼
Chlorine, 1 1½ trace.
------- ------- --------
100 100 100
Not only are the quantities of the several inorganic substances kinds
of straw very unlike—especially the proportions of potash, lime, and
phosphoric acid in each—but these quantities are also very different
from those exhibited by the numbers in the preceding table as contained
in the three varieties of grain. In this difference we see, further,
_one_ reason why the same soil which may be favourable to the growth
of straw may not be equally propitious to the growth of the ear. Wheat
straw contains little either of potash or of soda; the ash of the
grain contains a large proportion; while the ash of the oat-straw,
on the other hand, contains a much larger proportion of potash than
that of its own ear does. It is clear, therefore, that the roots may,
in certain plants and in certain soils, succeed in fully nourishing
the straw while they cannot fully ripen the ear; or contrariwise,
where they feed but a scanty straw, may yet _be able_ to give ample
sustenance to the filling ear.[8]
[8] And occasionally _do_ give; for a plump grain, and even a
well-filled ear, are not unfrequently found where the straw is
unusually deficient.
3. The quality of the ash varies also with the soil in which it grows.
This will be understood from what is stated above. Where the soil is
favourable, the roots can send up into the straw every thing which the
healthy plant requires; when it is poorly supplied with some of those
inorganic constituents which the plant desires, life may be prolonged,
a stunted or unhealthy crop may be raised, in which the kind, and
perhaps the quantity, of ash left in burning will necessarily be
different from that left by the same species of plant grown under more
favouring circumstances. Of this fact there can be no doubt, though
the extent to which such variations may take place without absolutely
killing the plant, has not yet been by any means made out.
4. It varies also with the period of a plant’s growth, or the season at
which it is reaped. Thus, in the young leaf of the turnip and potato,
a greater proportion of the inorganic matter they contain consists of
potash than in the old leaf. The same is true of the stalk of wheat;
and similar differences prevail in almost every kind of plant at
different stages of its growth.
The enlightened agriculturist will perceive that all the facts above
stated have a perceptible connection with the ordinary processes of
practical agriculture, and tend to throw considerable light on some of
the principles by which they ought to be regulated. One illustration of
this is exhibited in the following section.
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