SSSAJ Journal of Natural Resources and Life Sciences Education
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Published in Soil Sci Soc Am J 46:667-671 (1982)
© 1982 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Hydrodynamic Dispersion Involving Cationic Adsorption During Unsaturated, Transient Water Flow in Soil1

K. B. Laryea, D. E. Elrick and M. J. L. Robin2

ABSTRACT

The analysis of hydrodynamic dispersion of solutes during one-dimensional absorption (horizontal flow) of solution into soil columns is extended to solutes which interact with the soil particle surfaces. The exchange process involved is assumed to be instantaneous and is described by a nonlinear adsorption isotherm. The relevant equations are solved for the apparent longitudinal dispersion coefficient using a computer program written in system/360 CSMP.

Experiments with a clay loam soil indicated that when a concentrated solution of potassium chloride (KCl) (1N) infiltrates into a Ca2+-saturated soil, the apparent longitudinal dispersion coefficient is effectively velocity independent. This calculated coefficient reflects the possible combined effects of an immobile water fraction and salt exclusion.


NOTES

1 Contribution from the Dep. of Land Resource Science, Univ. of Guelph, Guelph, Ontario, Canada. The Authors acknowledge support from the Natural Sciences and Engineering Research Council of Canada and the Ontario Ministry of Agriculture and Food.

2 Visiting Lecturer, Professor, and Research Associate, respectively.

Received for publication August 19, 1981. Accepted for publication March 18, 1982.







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