Skip to main content
Log in

Decomposition of root exudates in soil

  • Published:
Folia Microbiologica Aims and scope Submit manuscript

Abstract

The conversion of synthetic root exudates, i.e. of a mixture of amino acids, organic acids and sugars, added to soil in a single dose or continuously, was studied. After the addition of a single dose, the root exudates were gradually mineralized and after 76 hours, 85% of carbon had been released in the form of carbon dioxide. The extent and rate of mineralization was not influenced by the simultaneous addition of ammonium phosphate. The continuous addition of substrate formed a model artificial rhizosphere. In the steady state, 93% of the carbon in the added substrate was mineralized to carbon dioxide. The conversion of organic acids, sugars and amino acids and the mineralization of nitrogen was studied simultaneously by chromatography. In soil continuously enriched with root exudates, phenomena similar to the rhizosphere effect in nature were observed both in the numbers of microorganisms and in the relative incidence of the nutritional groups of bacteria.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Bremner, J. M., Shaw, K.:Denitrification of soil. I. Methods of investigation. J. agr. Sci. 51:22, 1958.

    Article  CAS  Google Scholar 

  • Drobník, J.:A respirometric study of glucose metabolism in soil samples. Fol. biol. (Praha) 4: 137, 1958.

    Google Scholar 

  • Drobník, J.:A Warburg vessel for soil samples. Nature 188: 686, 1960a.

    Article  Google Scholar 

  • Drobník, J.:Primary oxidation of organic matter in the soil. I. The form of respiration curves with glucose as the substrate. Plant & Soil 12: 199. 1960b.

    Article  Google Scholar 

  • Drobník, J.:Primary oxidation of some organic compounds in remoistened air-dried soil. Can. J. Microbiol. 7: 769, 1961.

    PubMed  Google Scholar 

  • Lees, H., Quastel, J. H.:Biochemistry of nitrification in soil I. Kinetics of, and the effects of poisons on, soil nitrification, as studied by a soil perfusion technique. Addendum by H. Lees: A soil perfusion apparatus. Biochem. J. 40: 803, 1946.

    CAS  Google Scholar 

  • Macura, J.:Seed and soil bacteria in relation to the rhizosphere effect. Fol. biol. (Praha) 4: 274, 1958.

    Google Scholar 

  • Maoura, J.:Continuous flow method in soil microbiology. I. Apparatus. Fol. microbiol. 6: 328, 1961.

    Article  Google Scholar 

  • Macura, J.:Interrelations between microorganisms and plant in the rhizosphere. Plant Microbes Relationships. Proc. Symp. on Relationships between Soil Microorganisms and Plant Roots, p. 26. Publ. House Czechoslov. Acad. Sci., Prague, 1965.

    Google Scholar 

  • Macura, J., Kunc, F.:Continuous flow method in soil microbiology. II. Observations on glucose metabolism. Fol. microbiol. 6: 398, 1961.

    Article  CAS  Google Scholar 

  • Me Garity, J. W., Gilmour, C. M., Bollen, W. B.:Use of an electrolytic respirometer to study denitrification in soil. Can. J. Microbiol. 4: 303, 1958.

    Google Scholar 

  • Najmr, S., Cikánek, M.:Simultaneous determination of carbon and nitrogen in soil. (In Czech). Sborník ČSAZV A. 26: 285, 1953.

    Google Scholar 

  • Novák B., Nováková, J.:The effect of organic materials on physical, chemical and microbiological changes of soil with particular regard to humus formation. (In Czech). Rostlinná výroba. 6: 1399, 1960.

    Google Scholar 

  • Rivière, J.:Etude de la rhizosphère du blé. Ann. Agronomique 11: 397, 1960.

    Google Scholar 

  • Rovira, A. D.:Plant root excretions in relation to the rhizosphere effect. II. A study of the properties of root exudates, its effect on the growth of microorganisms isolated from the rhizosphere and control soil. Plant & Soil, 7: 195, 1956.

    Article  Google Scholar 

  • Schmidt, E. L., Putnam, H. D., Paul, E. A.:Behaviour of amino acids in soil. Bacteriol. Proc. p. 11, 1957.

  • Sasson, A., Kunc, F.:Sur l’activité biologique de sols arides du Maroc. Bulletin de la Société des Sciences Naturelles et Physiques du Maroc, 1er et 2me trimestres. 55, 1963.

  • Smith, N. R., Dawson, V. T.:The bacteriostatic action of bengal rose in media used for plate counts of soil fungi. Soil Sci. 58: 467, 1944.

    Article  CAS  Google Scholar 

  • Stotzky, G.:A simple method for the determination of the respiratory quotient of soils. Can. J. Microbiol. 6: 439, 1960.

    Article  PubMed  CAS  Google Scholar 

  • Stotzky, G., Norman, A. G.:Factors limiting microbial activities in soil. I. The level of substrate, nitrogen and phosphorus. Arch. Mikrobiol. 40: 341, 1961.

    Article  PubMed  CAS  Google Scholar 

  • Taylor, C. B.:The nutritional requirements of predominant flora of the soil. Proc. Soc. appl. Bact. 14:: 101, 1951.

    Google Scholar 

  • Timonin, M. J.:The interaction of higher plants and soil microorganisms. III. Effect of by-products of plant growth on activity of fungi and actinomycetes. Soil Sci. 52: 395, 1941.

    Article  Google Scholar 

  • Vancura, V.:Root exudates of plants. I. Analysis of root exudates of barley and wheat in their initial phases of growth. Plant & Soil 21: 231, 1964.

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Kunc, F., Macura, J. Decomposition of root exudates in soil. Folia Microbiol 11, 239–247 (1966). https://doi.org/10.1007/BF02878892

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02878892

Keywords

Navigation