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
It was thus clearly proved that _A. vinelandii_ at
least does not need symbiosis with algæ to fix atmospheric
nitrogen; but experiments with mixed cultures of the above
bacillus and another (designated as No. 30 by Lipman) proved
that when these two co-operate the absorption of atmospheric
nitrogen is nearly doubled. As it is probable that this is
the case also with other soil bacteria, the importance of
this source of nitrogen to plants is obvious; provided of
course that the proper nutritive ingredients are present
in available form. Lipman shows that among the organic
nutrients, besides the sugars, glycerine and the salts of
propionic and lactic acids, and probably also others of the
same groups, can serve as nourishment to the nitrogen-fixing
bacteria.
DISTRIBUTION OF THE HUMUS WITHIN THE SURFACE SOIL.
The uniform distribution of the humus-contents of the surface soil, as
shown in sections of the same, is by no means easily accounted for.
The roots from which its substance is so largely derived are not so
universally distributed as to account for it; but least of all can the
rapid disappearance of the leaf-fall and other vegetable offal from
the surface be accounted for without some outside agencies. Of these,
the action of fungous vegetation, and of insects and earthworms, are
doubtless the chief ones.
_Fungi._—When we examine a decaying root, we find radiating from it
a zone of deeper tint, as though from a colored solution penetrating
outward. But since under normal conditions humus is insoluble, this
explanation cannot stand. Microscopic examination, however, reveals
that the outside limit of this zone is also the limit to which the
fungous fibrils concerned in the process extend; and as these fibrils
are much more finely distributed and much more numerous than the
roots of any plant, it is natural that the humus resulting from
their decomposition should be more evenly distributed than the roots
themselves.[62]
[62] Kosticheff, Formation and Properties of Humus; in abstract Jour.
Chem. Soc., 1891, p. 611.
Such fungous growth is not, however, confined to dead and decaying
roots only. A large number of trees and shrubs, among them pines and
firs, beeches, aspen and many others, also the heaths, and woody plants
associated with them, appear to depend largely for their healthy
development, notably in northern latitudes, upon the co-operation
(“symbiosis”) of fungous fibrils that “infest” their roots, enabling
them to assimilate, indirectly, the decaying organic (and inorganic)
matter which would otherwise be unavailable, and at the same time
converting that matter into their own substance. Fungous growths thus
mediate both the decomposition and rehabilitation of the vegetable
debris.
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