The micro-organisms of the soilRussell, Edward J. (Edward John)
Science
The micro-organisms of the soil
Russell, Edward J. (Edward John)
Soil microbiology
These transformations of energy involve transformations of matter.
The original plant residues may be divided roughly into substances
forming the structure of the plant, such as the hemicelluloses, the
pentosans, gums, and the contents of the cell--the protoplasm and the
storage products, protein; in addition, there are smaller quantities of
fats and waxes and other constituents. Some of the easily-decomposable
carbohydrates never reach the soil at all, being broken down by
intracellular respiration or attack of micro-organisms. But much of the
structure material--hemicelluloses, pentosans, etc.--remains.
Once the plant residues pass through the earthworm bodies they become
completely disintegrated and lose all signs of structure.
The only visible product so far known is humus, the black sticky
substance characteristic of soil and of manure. Two modes of formation
have been suggested. Carbohydrates, sugars, pentosans, etc., are
known to yield furfuraldehyde or hydroxymethylfurfuraldehyde on
decomposition, and it has been shown at Rothamsted that this readily
condenses to form a humus-like body, if not humus itself. In the
laboratory the reaction is effected in presence of acid, but even
amino-acids suffice. All the necessary conditions occur in the soil,
and humus formation may proceed in this way.
Some of the structure material--the lignin--contains aromatic ring
groupings. Fischer and Schrader have shown that in alkaline conditions
these ring substances absorb oxygen and form something very like humus.
It is quite possible that humus formation also proceeds in the soil
in this way. Whether the two products are chemically identical is not
known.
The scheme can be represented thus:--
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