Presence and oxidation of amino acids in rhizosphere and non-rhizosphere soil

Manometric studies were carried out on the respiratory activity of different rhizosphere and non-rhizosphere soils to follow quantitatively the over-all microbial activity in the rhizosphere soil as affected by the species and growth phase of plant. Oxygen consumption was distinctly greater in rhizosphere soils as compared to that in non-rhizosphere soils. The difference between oxygen consumption by rhizosphere and non-rhizosphere soils changed with the course of plant growth and it was not the same in different plants. This difference in oxygen consumption might be a measure of the amount of available oxidizable substrate in the rhizosphere. A rhizosphere sample had greater diversity as well as higher concentration of free amino acids than a non-rhizosphere sample of the same soil. Bacterial counts pointed to preferential stimulation in the rhizosphere of bacteria requiring individual amino acids. amino acids, such as glycine, alanine, asparsic acid of tyrosine were oxidized more rapidly in rhizosphere than in non-rhizosphere soil, but the extsent of oxidation for each of the amino acids studied did not differ. The amount of oxygen consumed during oxidation of alanine, aspartic acid or tyrosine was about one-half of the total amount necessary for complete oxidation. With glycine a higher extent of oxidation (60%) was observed. These extents of oxidation of glycine and aspartic acid did not change on investigation at two different phases of plant growth.