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Three-dimensional analysis of infiltration from the disc infiltrometer: 1. A capillary-based theory
Journal article   Open access   Peer reviewed

Three-dimensional analysis of infiltration from the disc infiltrometer: 1. A capillary-based theory

K.R.J. Smettem, J.Y. Parlange, P.J. Ross and R. Haverkamp
Water Resources Research, Vol.30(11), pp.2925-2929
1994
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Abstract

The hydraulic properties of an unsaturated homogenous and isotropic soil can be obtained from the unconfined flux out of a disc infiltrometer into the soil over the depth of wetting. The disc infiltrometer is becoming increasingly popular, but methods of analysis have generally relied on the restrictive assumptions of one-dimensional flow at early times or quasi-steady state flow at large times. We provide an approximate analytical expression for three-dimensional unsteady, unconfined flow out of a disc infiltrometer, and this includes the geometric effect of the circular source but ignores gravity. This physically based solution is tested against data obtained from laboratory experiments on repacked material. The results illustrate that the difference between three-dimensional and one-dimensional flow is linear with time.

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Collaboration types
Domestic collaboration
International collaboration
Citation topics
3 Agriculture, Environment & Ecology
3.45 Soil Science
3.45.879 Soil Erosion
Web Of Science research areas
Environmental Sciences
Limnology
Water Resources
ESI research areas
Environment/Ecology
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