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
_Ammonia-forming Bacteria._—A large number of different bacteria appear
to be concerned in the formation of ammonia from compounds of the
albuminoid group, (and probably from humus). Among these is one of the
most common in soils (_Bacillus mycoides_, root bacillus), which while
forming ammonia carbonate in solutions of albumen, is also capable of
reducing nitrates to nitrites and ammonia in presence of a nutritive
solution of sugar.
The “hay bacillus” (_B. subtilis_), so abundantly developed in hay
infusions, and one of the most abundant in cultivated soils, has
together with B. ellenbachensis, B. megatherium, B. mycoides, and
others, by some been credited with important action in favoring
vegetation; so that a fairly pure culture of B. ellenbachensis has
been brought out commercially in Germany under the name of “Alinit.”
Rigorous culture experiments made by Stutzer and others have,
however, failed to show any general benefit from the use of alinit in
infecting either land or seeds. But there is no doubt of the _Effects
of Bacterial Life on Physical Soil Conditions._—It is apparent that
all conditions favoring the life of aerobic (air-needing) bacteria
tend also to produce the loose, porous state (tilth) of the surface
soil so conducive to the welfare of culture plants, designated by
German agriculturists as “Bodengare.” Whether or not this condition is
directly due to bacterial processes, as is thought by Stutzer (Landw.
Presse, 1904, No. 11) it is assuredly a highly important point to
be gained, and is essentially connected with the presence of humus
in adequate amounts, which is also a favoring condition of abundant
bacterial life. It seems that the preference given to the shallow
putting-in, or even surface application of stable manure, existing in
Europe, is largely based upon the marked effect upon the looseness of
the surface soil, generally credited to the physical effect of the
manure substance itself, but apparently largely due to the intensity of
bacterial action thus brought about.
[Illustration: FIG. 18.—Bacillus subtilis. (Wollny, after Brefeld.)]
[Illustration: FIG. 19.—Bacteria producing ammoniacal fermentation:
_A_, _C. mycoides_: _B_, _B. stutzeri_. (From Conn, Agr. Bacteriology.)]
[Illustration: FIG. 20.—Bacillus megaterium. (From Migula.)]
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