Abstract
NITRIFICATION of ammonium ions to nitrite and thence to nitrate is commonly a rapid process in soil; yet the isolation of the organisms responsible has always proved to be a difficult and tedious procedure. The reason for this is not difficult to find. The work of Winogradsky and of Meyerhof, which has been summarized in her book by the late Dr. Stephenson1, has shown that the nitrifying organisms (Nitrosomonas and Nitrobacter) consume rather more than a hundred atoms of oxygen for every atom of carbon assimilated. On the other hand, the generality of (heterotrophic) soil organisms consumes only about five atoms of oxygen for every atom of carbon assimilated, according to the results of experiments on the carbon dioxide outputs of soils2; this latter result of Porteous and Lees has been confirmed by as yet unpublished measurements of the oxygen uptakes of soils in the percolating respirometer3.
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References
Stephenson, M., “Bacterial Metabolism” (Longmans, Green and Co., London, 1949).
Lees, H., and Porteous, J. W., Plant and Soil, 2, 231 (1950).
Lees, H., Nature, 166, 118 (1950).
Höber, R. (edit.), “The Physical Chemistry of Cells and Tissues” (Churchill, London, 1945).
Lees, H., Plant and Soil, 1, 221 (1949).
Meiklejohn, J., J. Gen. Microbiol., 4, 185 (1950).
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LEES, H. Isolation of the Nitrifying Organisms from Soil. Nature 167, 355–356 (1951). https://doi.org/10.1038/167355b0
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DOI: https://doi.org/10.1038/167355b0
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