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
_Blood_ is rarely applied to the land directly—though, like the other
parts of animals, it makes an excellent compost. As it comes from
the sugar refineries, however, in which, with lime water and animal
charcoal, it is employed for the refining of sugar, it has obtained
a very extensive employment, especially in the south of France. This
animal black, or _animalized charcoal_, as it is sometimes called,
contains about twenty per cent. of blood, and has risen to such a price
in France, that the sugar refiners actually sell it for more than the
unmixed blood and animal charcoal originally cost them. This has given
rise to the manufacture of artificial mixtures of charcoal, fecal
matters, and blood, which are also sold under the name of animalized
charcoal. The only disadvantage attending these artificial preparations
is, that they are liable to be adulterated, or, for cheapness, prepared
in a less efficient manner.
_Horn_, _hair_, and _wool_, depend for their efficacy precisely on the
same principles as the blood and flesh of animals. They differ chiefly
in this, that they are _dry_, while blood and flesh contain 80 to 90
per cent. of their weight of water. Hence, a ton of horn shavings, of
hair, or of dry woollen rags, ought to enrich the soil as much as ten
tons of blood. In consequence, however, of their dryness, the horn and
wool decompose much more slowly than the blood. Hence, the effect of
soft animal matters is more immediate and apparent, that of hard and
dry substances less visible, but continuing for a much longer period of
time.
_Bones_, again, while they resemble horn in being dry, differ from it
in containing, besides the animal matter, a large quantity of earthy
matter also, and hence they introduce a new agent to aid their effect
upon the soil. Thus, the bones of the cow consist of 100 lbs. of
Phosphate of lime, 55½
Phosphate of magnesia, 3
Soda and common salt, 3½
Carbonate of lime, 3¾
Fluoride of calcium, 1
Gelatine (the substance of _horn_), 33¼
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100
While 100 lbs. of bone-dust, therefore, add to the soil as much
_organic_ animal matter as 33 lbs. of horn, or as 300 or 400 lbs.
of blood or flesh, they add, at the same time, much _inorganic_
matter—lime, magnesia, soda, common salt, and phosphoric acid (in
the phosphates),—all of which, as we have seen, must be present in a
fertile soil, since the plants require a certain supply of them all
at every period of their growth. These substances, like the inorganic
matter of plants, may remain in the soil, and may exert a beneficial
action upon vegetation after all the organic or gelatinous matter has
decayed and disappeared.
From what is above stated, therefore, the reader will gather these
general conclusions:
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