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
Such marked _increases_ from soil inoculation cannot of course be
expected in cases where the soil has previously borne leguminous crops
of similar nature and therefore already contains the root bacteria.
Hence Duggar found no increase of production when inoculating for
cowpea, land that had borne that crop two years before and already
contained the root bacteria. In the arid region, where the almost
universally calcareous soils usually bear a natural growth largely
composed of various leguminous plants, inoculation is likely to be less
commonly effective than in the humid region east of the Mississippi,
where leguminous plants are much less generally present in the native
flora.
The distinctive agricultural function of supplying nitrogen to the
soils on which they grow, renders inexcusable the persistence of some
writers and teachers in designating all forage plants as “grasses.”
Whatever excuse there may have been for this practice so long as the
nitrogen-gathering function of the legumes was unknown, disappears
with this discovery, and the misleading misnomer should be banished
from agricultural publications and lectures, at the very least.
_Other Nitrogen-Absorbing Bacteria._—An increase in the
nitrogen-content of some soils, aside from the action of leguminous
root-bacteria, has long been observed. As already stated, this increase
was at first ascribed to certain green algæ often seen to develop on
the soil surface; but it has now been shown that the nitrogen-gathering
function belongs to at least two bacteria, one of which (_Clostridium
pastorianum_) was discovered by Winogradski, the other (_Azotobacter
chroococcum_) by Beyerinck, and has since been farther investigated by
Koch, Kröber, Gerlach and Vogel, and last by Lipman and Hugo Fischer.
According to the latter it seems likely that Azotobacter chroococcum
lives in symbiosis with the green algæ, all of which, like the
Azotobacter itself, develop with special luxuriance on calcareous soils.
Lipman (Rep. Agr. Exp’t Station, New Jersey, 1903 and 1904)
describes as _Azotobacter vinelandii_ a form somewhat
different from the A. chroococcum, the nitrogen-assimilating
power of which he tested quite elaborately. He exposed to
air pure cultures of _A. vinelandii_ in nutritive
solution containing the proper mineral ingredients, and
glucose 20 grams per liter. 100 cub. centimeters of this
solution was exposed in flasks of respectively 250, 500
and 1000 cc. content, therefore having greater surface in
the larger flasks. After ten days, the amounts of nitrogen
fixed were found to be respectively 1.67, 3.19 and 7.90
milligrams. When mannite solution was employed instead of
glucose, a similar fixation was observed; and it was also
shown that the presence of combined nitrogen in the forms of
nitrates or ammonium salts discouraged the fixation by the
bacillus.
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