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Separation of Sub-Micron Particles from Soils and Sediments without Mechanical Disturbance

Published online by Cambridge University Press:  28 February 2024

G. J. Churchman
Affiliation:
CSIRO Division of Soils, and Australian Cooperative Research Centre for Soil and Land Management, Private Bag No. 2, Glen Osmond, South Australia 5064
D. A. Weissmann
Affiliation:
CSIRO Division of Soils, and Australian Cooperative Research Centre for Soil and Land Management, Private Bag No. 2, Glen Osmond, South Australia 5064

Abstract

A method is described for the separation of the finest particles from soils and sediments without mechanical disturbance. Particles are separated through the induction of osmotic stress. Generally, samples are treated with a concentrated sodium salt solution and then exposed to water by diffusion. Naturally sodic samples are simply exposed to water. Solid samples and the swollen and dispersed material they produce are confined by dialysis tubing. Examples show that the method gives a size gradient of particles in a vertical column of suspension. The compositions of particles can vary with size. The method can be used to show the effects on separated particles of ions other than Na+ and also of other physicochemical treatments of soils and sediments. It is inexpensive and requires little labor.

Type
Research Article
Copyright
Copyright © 1995, The Clay Minerals Society

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References

Churchman, G. J., and Foster, R. C. 1994 . The role of clay minerals in the maintenance of soil structure. Trans. 15th World Congr. Soil Sci. 8a: 1734.Google Scholar
Churchman, G. J., and Oades, J. M. Interparticle bonding by organic matter and metal oxides: Effects on swelling. In Clay Swelling and Expansive Soils. Baveye, P., and McBride, M. B., 1995 eds. Dordrecht: Kluwer (in press).Google Scholar
Churchman, G. J., and Weissmann, D. A. Particle mobility as a parameter in soil dispersibility. In Distribution, Properties and Management of Australian Sodic Soils. Naidu, R., Sumner, M. E., and Rengasamy, P., 1995 eds. Melbourne: CSIRO (in press).Google Scholar
Churchman, G. J., Slade, P. G., Self, P. G., and Janik, L. J. 1994 . Nature of interstratified kaolin-smectites in some Australian soils. Aust. J. Soil Res. 32: 805822.CrossRefGoogle Scholar
Clapp, C. E., and Emerson, W. W. 1965 . The effect of periodate oxidation on the strength of soil crumbs. Soil Sci. Soc. Amer. Proc. 29: 127130.CrossRefGoogle Scholar
Cradwick, P. D., and Wilson, M. J. 1972 . Calculated X-ray diffraction profiles for interstratified kaolinite-montmorillonite. Clay Miner. 9: 395405.CrossRefGoogle Scholar
Emerson, W. W., 1954. The determination of the stability of soil crumbs. J. Soil Sci. 5: 233250.CrossRefGoogle Scholar
Gupta, R. K., and Abrol, I. P. 1990 . Salt-affected soils: their reclamation and management for crop production. Adv. Soil Sci. 11: 223288.CrossRefGoogle Scholar
Northcote, K. H., and Skene, J. K. M. 1972 . Australian soils with saline and sodic properties. CSIRO Australia Soil Publication No. 27.Google Scholar
Robert, M., and Chenu, C. Interactions between soil minerals and microorganisms. In Soil Biochemistry, Vol. 7. Stotzky, G., & Bollag, J.-M., 1992 eds. New York: Marcel Dekker, 307404.Google Scholar
Shainberg, I., and Letey, J. 1984 . Response of soils to sodic and saline conditions. Hilgardia 52: 157.CrossRefGoogle Scholar
Stace, H. C. T., Hubble, G. D., Brewer, R., Northcote, K. H., Sleeman, J. R., Mulcahy, M. J., and Hallsworth, E. G. 1968 . A Handbook of Australian Soils. Glenside, South Australia: Rellim, 435 pp.CrossRefGoogle Scholar