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The effect of the nutrient intensity and buffering power of a soil, and the absorbing power, size and root hairs of a root, on nutrient absorption by diffusion

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Summary

A portion of a single plant root is treated as an absorbing cylindrical sink to which nutrients move by diffusion. Assuming that the rate of uptake of nutrient is proportional to its concentration at the root surface, and that the nutrient, though reacting with the solid, moves only through the soil solution, standard diffusion equations are used to calculate the effect of soil and plant characteristics on the rate of uptake. The treatment is applicable to phosphorus and potassium. Among soil properties uptake should increase directly with the soil solution concentration. It should also increase, but only slowly, with increasing buffering power. It increases with increasing soil moisture. Among plant characteristics, uptake should increase with the root absorbing power until diffusion through the soil becomes limiting. Absorption by unit surface area of root increases as the root radius decreases. A root hair is shown to interfere quickly with the uptake of adjacent hairs. The hairs increase absorption by the root because they can exploit rapidly the soil between the hairs, and they have the effect of extending the effective root surface to their tips.

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References

  1. Barber, S. A., Walker, J. M. and Vasey, E. H., Principles of ion movement through the soil to the plant root. Intern. Soil. Conf. New Zealand, 121–124 (1962).

  2. Beckett, P. H. T., Studies on soil potassium II. The ‘immediate’ Q/I relations of labile potassium in the soil. J. Soil Sci.15 9–23 (1964).

    Google Scholar 

  3. Blanchet, R., Relations entre la vitesse de dilution isotopique du phosphore du sol et l'alimentation phosphatée des plantes. Compt. Rend.244 2739–2741 (1957).

    Google Scholar 

  4. Bouldin, D. R., Mathematical description of diffusion processes in the soil-plant system. Soil Sci. Soc. Am. Proc.25 476–480 (1961).

    Google Scholar 

  5. Carslaw, M. S. and Jaeger, J. C., Conduction of Heat in Solids-(2nd Edition) Oxford (1959).

  6. Crank, J., The Mathematics of Diffusion, Oxford (1956).

  7. Dittmer, H. J., A quantitative study of the subterranean members of soyabean. Soil Cons.6 33–34 (1940).

    Google Scholar 

  8. Gardner, W. R., Dynamic aspects of water availability to plants. Soil Science89 63–73 (1960).

    Google Scholar 

  9. Kramer, P. J. and Coile, T. S., An estimation of the volume of water made available by root extension. Plant Physiol.15 743–747 (1940).

    Google Scholar 

  10. Lewis, D. G. and Quirk, J. P., Diffusion of phosphate in soil. Intern. Soil Conf. New Zealand 132–138 (1962).

  11. Mattingly, G. E. G., Russell, R. D. and Jephcott, B. M., Experiments on cumulative dressings of fertilizers on calcareous soils in South-West England. II — Phosphorus uptake by Ryegrass in the greenhouse. J. Sci. Food and Agr.9 629–637 (1963).

    Google Scholar 

  12. Moss, P., Some aspects of the cation status of soil moisture. Pt. I. The ratio law and moisture content. Plant and Soil18 99–113 (1963).

    Google Scholar 

  13. Nye, P. H., Soil analysis and the assessment of fertility in tropical soils. J. Sci. Food and Agr.14 277–280 (1963).

    Google Scholar 

  14. Nye, P. H., The measurement and mechanism of ion diffusion in soils. I. The relation between self-diffusion and bulk diffusion. J. Soil Sci.17 16–23 (1966).

    Google Scholar 

  15. Nye, P. H. and Spiers, J. A., Simultaneous diffusion and mass flow to plant roots. Trans. 8th Intern Congr. Soil Sci. Bucharest (1964) (in press).

  16. Olsen, S. R., Kemper, W. D. and Jackson, R. D., Phosphate diffusion to plant roots. Soil Sci. Soc. Am. Proc.26 222–227 (1962).

    Google Scholar 

  17. Passioura, J. B., A mathematical model for the uptake of ions from the soil solution. Plant and Soil18 225–238 (1963).

    Google Scholar 

  18. Porter, L. K., Kemper, W. D., Jackson, R. D. and Stewart, B. A., Chloride diffusion in soils as influenced by moisture content. Soil Sci. Soc. Am. Proc.24 460–463 (1960).

    Google Scholar 

  19. Russell, R. S., Martin, R. P. and Bishop, O. N., A study of the absorbtion and utilization of phosphate by young barley plants. III — The relationship between external concentration and the absorbtion of phosphate. J. of Exptl. Botany5 327–342 (1954).

    Google Scholar 

  20. Scott, F. M., Root hair zone of soil grown roots. Nature199 1009–1010 (1963).

    Google Scholar 

  21. Wiersum, L. K., Utilization of soil by the plant root system. Plant and Soil15 189–191 (1961).

    Google Scholar 

  22. Williams, E. G., Chemical soil tests as an aid to increased productivity. Intern. Soil Conf. New Zealand, 820–834 (1962).

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Nye, P.H. The effect of the nutrient intensity and buffering power of a soil, and the absorbing power, size and root hairs of a root, on nutrient absorption by diffusion. Plant Soil 25, 81–105 (1966). https://doi.org/10.1007/BF01347964

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  • DOI: https://doi.org/10.1007/BF01347964

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