Scientific American Supplement, No. 470, January 3, 1885Various
Science
Scientific American Supplement, No. 470, January 3, 1885
Various
Science -- Periodicals
Some very practical conclusions may be drawn from the facts now stated. It
appears that the oxidation of nitrogenous matter in soil will be confined
to matter near the surface. The nitrates found in the subsoil and in
subsoil drainage waters have really been produced in the upper layer of
the soil, and have been carried down by diffusion, or by a descending
column of water. Again, in arranging a filter bed for the oxidation of
sewage, it is obvious that, with a heavy soil lying in its natural state
of consolidation, very little will be gained by making the filter bed of
considerable depth; while, if an artificial bed is to be constructed, it
is clearly the top soil, rich in oxidizing organisms, which should be
exclusively employed.
_The Substances Susceptible of Nitrification._--The analyses of soils and
drainage waters have taught us that the nitrogenous humic matter resulting
from the decay of plants is nitrifiable; also that the various nitrogenous
manures applied to land, as farmyard manure, bones, fish, blood, rape
cake, and ammonium salts, undergo nitrification in the soil. Illustrations
of many of these facts from the results obtained in the experimental
fields at Rothamsted have been published by Sir J.B. Lawes, Dr. J.H.
Gilbert, and myself, in a recent volume of the _Journal_ of the Royal
Agricultural Society of England. In the Rothamsted Laboratory, experiments
have also been made on the nitrification of solutions of various
substances. Besides solutions containing ammonium salts and urea, I have
succeeded in nitrifying solutions of asparagine, milk, and rape cake.
Thus, besides ammonia, two amides, and two forms of albuminoids have been
found susceptible of nitrification. In all cases in which amides or
albuminoids were employed, the formation of ammonia preceded the
production of nitric acid. Mr. C.F.A. Tuxen has already published in the
present year two series of experiments on the formation of ammonia and
nitric acids in soils to which bone-meal, fish-guano, or stable manure had
been applied; in all cases he found the formation of ammonia preceded the
formation of nitric acid.
As ammonia is so readily nitrifiable, we may safely assert that every
nitrogenous substance which yields ammonia when acted upon by the
organisms present in soil is also nitriflable.
_Certain Conditions having Great Influence in the Process of
Nitrification._--If we suppose that a solution containing a nitrifiable
substance is supplied with the nitrifying organism, and with the various
food constituents necessary for its growth and activity, the rapidity of
nitrification will depend on a variety of circumstances:
1. The degree of concentration of the solution is important. Nitrification
always commences first in the weakest solution, and there is probably in
the case of every solution a limit of concentration beyond which
nitrification is impossible.
2. The temperature has great influence. Nitrification proceeds far more
rapidly in summer than winter.
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