The Fundamentals of BacteriologyMorrey, Charles Bradfield
Science
The Fundamentals of Bacteriology
Morrey, Charles Bradfield
Bacteriology
There are also types of “free-living,” as distinguished from these
symbiotic, bacteria which absorb the free nitrogen of the air and aid
materially in keeping up this supply under natural conditions. One
of the most important of these types is the aërobic “Azotobacter”
(Fig. 76), while another is the anaërobic _Clostridium pasteurianum_.
The nitrogen which is absorbed is built up into the protein material
of the cell body and this latter must in all probability be “worked
over” by various types of decomposition bacteria and by the nitrous
and nitric organisms and be converted into utilizable nitrates just
as other protein material is, as has been discussed in Chapter X. At
any rate there is as yet no definite knowledge of any other method of
transformation. Up to the present no intentional practical utilization
of this valuable property of these free-living forms has been made.
=Nitrogen Nutrition of Green Plants.=--It is the belief of botanists
that green plants obtain their nitrogen chiefly in the form of
nitrates, though ammonium salts may be utilized to some extent by
certain plants at least. Exceptions to this general rule are those
plants provided with root tubercles (and the bog plants and others
which have mycorrhiza?). These plants obtain their nitrogen in the
form of organic compounds made for them by the bacteria growing in
the tubercles. That nitrogen circulates throughout the structure of
plants in organic combination is certain. There does not appear to
be any reason why similar compounds which are soluble and diffusible
(amino-acids?) should not be taken up through the roots of plants and
utilized as such. _It seems to the author that this is very probably
the case._ Arguments in favor of this view are: (1) The nitrogen
nutrition of leguminous and other plants with root nodules. (2) The
close symbiosis between “Azotobacter” and similar nitrogen-absorbing
bacteria and many species of algæ in sea water at least. (3) The
vigorous growth of plants in soils very rich in organic matter, which
inhibits the production of nitrates by the nitrous-nitric bacteria
when grown in culture, and possibly (?) in the soil, so that nitrates
may not account for the vigorous growth. (4) The effect of nitrate
fertilizers is to add an amount of nitrogen to the crop much in excess
of the amount added as nitrate. (5) The most fertile soils contain
the largest numbers of bacteria. The doctrine that nitrates furnish
the only nitrogen to plants was established before the activities of
bacteria in the soil were suspected, and, so far as the author is
aware, has not been supported by experiments under conditions rigidly
controlled as to sterility.
It would seem that one of the chief functions of soil bacteria is to
prepare soluble organic compounds of nitrogen for the use of green
plants and thus to make a “short cut” in the nitrogen cycle (p. 107),
as now believed in, direct from the “decomposition bacteria” to green
plants.
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