Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
_Functions of the Bacteria._—While there is still much uncertainty as
to the exact functions performed by most of these bacteria in respect
to soil-formation and plant growth, there are several kinds whose
activity has been proved to be of the utmost importance in one or both
directions; it having been shown that when the soil is sterilized
either by heat or antiseptic agents, certain essential processes are
completely suppressed until the soil is re-infected and the conditions
of bacterial life restored.
Probably the chief in importance are those connected with the processes
of _nitrification_ and _denitrification_, bearing as they do upon the
supply to plants of the most costly of the three substances furnished
by fertilizers. These organisms have been first extensively studied by
Winogradsky, while the conditions of their activity have been largely
developed by R. Warington.
[Illustration: FIG. 15.—Nitrosomonas. (Winogradsky).]
[Illustration: FIG. 16.—Nitrobacterium. (Winogradsky).]
_Nitrifying Bacteria._—The conversion of ammonia into nitrates is
accomplished under proper conditions by two organisms, or groups of
organisms; the first stage being the formation of nitrites by the
round, often flagellate cells of _nitrosomonas_ (or nitrosococcus).
The second, the oxidation of the nitrites into nitrates by very minute
rod-shaped bacilli, named _nitrobacteria_. The conditions under which
these bacteria can act are quite definite in that, aside from a supply
of the nitrifiable substance, a fairly high temperature (24° C. or 75°
F.) and a moderate degree of moisture, there must be a free access of
oxygen (air); and there must be present a base (or its carbonate) with
which the acids formed by oxidation can immediately unite. In an acid
medium (“sour” soils) nitrification promptly ceases; as it also does
whenever the amount of base present has been fully neutralized. The
bases most favorable to nitrification are lime and magnesia in the form
of carbonates, an excess of which does no harm; while in the case of
the carbonates of potash and soda, the amount must be strictly limited.
_Conditions of Activity._—Dumont and Crochetelle found
that up to .25 per cent, potassic carbonate acted favorably
on the process; which was, however, completely stopped by
as much as .8 per ct. Warington has shown that ammonic
carbonate similarly prevents nitrification when exceeding
about .37 per ct. Ammonia salts in general appear to be
antagonistic to the transformation of nitrites into nitrates.
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