Skip to main content
Log in

Cation exchange properties of plant root surfaces

  • Published:
Plant and Soil Aims and scope Submit manuscript

Summary

Plant roots show the “suspension effect” and interact with neutral salts with the development of exchange acidity, thus indicating the existence of a cation double layer associated with root surface. Plant root surfaces possess cation exchange capacities which may be measured by the adsorption and release of various cations. H-ions are associated with root surfaces in exchangeable form, and may be replaced by other cations.

These phenomena do not depend directly upon root metabolism, since the same results are obtained at 0°C and 25°C, with living roots and with ether-killed roots.

Entry of cations into the root double layer follows the type of lyotropic series observed with many inorganic and organic exchange materials. The lyotropic series, in decreasing order of replacing ability is:

$$H^ + > Ba^{ + + } > Ca^{ + + } > Mg^{ + + } > Cs^ + > Rb^ + > NH_4 ^ + > K^ + > Na^ + > Li^ + .$$

Root tips and root hair zones are the most active root portions insofar as surface exchange properties are concerned.

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

  1. Gieseking, J. E. and Jenny, Hans, Behavior of polyvalent cations in base exchange. Soil Sci.42, 273–280 (1936).

    Google Scholar 

  2. Hoagland, D. R. and Broyer, T. C., Accumulation of salt and permeability in plant cells. Jour. Gen. Physiol.25, 865–880 (1942).

    Google Scholar 

  3. Jacobson, Louis and Overstreet, Roy, A study of the mechanism of ion absorption by plant roots using radioactive elements. Amer. Jour. Bot.34, 415–420 (1947).

    Google Scholar 

  4. Jenny, Hans, Contact phenomena between adsorbents and their significance in the mineral nutrition of plants. Plant Nutrition Symposium, University of Wisconsin Press, 1949.

  5. Lundegårdh, Henrik, Investigations as to the absorption and accumulation of inorganic ions. Ann. Agric. Col. Sweden8, 234–404 (1940).

    Google Scholar 

  6. Mehlich, A., Determination of cation- and anion-exchange properties of soils. Soil Sci.66, 429–445 (1948).

    Google Scholar 

  7. Stewart, F. E., Prevot, C. P., and Harrison, J.A., Absorption and accumulation of rubidium bromide by barley roots-Localization in the root of cation accumulation and of transfer to the shoot. Plant Physiol.17, 411–421 (1942).

    Google Scholar 

  8. Wiegner, G., Some physico-chemical properties of clays. Soc. of Chem. Ind.50 55–71 (1931).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Additional information

Assistant Soil Chemist, A. E. C. Research Fellow, respectively. Assistance of T. R. Nielsen with many of the analyses is acknowledged.

The authors are indebted to Professor Hans Jenny for initiating this study and for his interest and advice throughout the investigation.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Williams, D.E., Coleman, N.T. Cation exchange properties of plant root surfaces. Plant Soil 2, 243–256 (1950). https://doi.org/10.1007/BF01852352

Download citation

  • Received:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF01852352

Keywords

Navigation