Technical Papers
Aug 20, 2012

Effect of the Capillary Fringe on Steady-State Water Tables in Drained Lands. II: Effect of an Underlying Impermeable Bed

Publication: Journal of Irrigation and Drainage Engineering
Volume 139, Issue 4

Abstract

A tension-saturated capillary fringe above the water table in drained lands gives rise to lower water tables than would occur in its absence. Results of a conformal mapping solution for the flow from uniform steady rainfall rates on the soil surface to deep drains installed above an impermeable bed when the soil above the drains is wholly tension-saturated show that the effect on the water table is greater the nearer the drain is to the impermeable floor. The effect becomes less with increasing rainfall rate. For the very deep tension-saturated soils assumed in the analysis (that implies a very large negative value for the air-entry pressure for the soil), the results obtained give lower bounds for the water-table heights in real soils with finite air-entry values that lie between the calculated ones and those obtained by theory neglecting a capillary fringe.

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References

Childs, E. C. (1945). “The water table, equipotentials and streamlines in drained lands: III.” Soil Sci., 59(5), 405–415.
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Go to Journal of Irrigation and Drainage Engineering
Journal of Irrigation and Drainage Engineering
Volume 139Issue 4April 2013
Pages: 309 - 312

History

Received: Oct 4, 2011
Accepted: Aug 8, 2012
Published online: Aug 20, 2012
Published in print: Apr 1, 2013

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Authors

Affiliations

E. G. Youngs [email protected]
Visiting Research Professor, Dept. of Environment, Earth and Ecosystems, Open Univ., Walton Hall, Milton Keynes MK7 6AA, UK. E-mail: [email protected]

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