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Three-dimensional analysis of infiltration from the disc infiltrometer: 2. Physically based infiltration equation
Journal article   Open access   Peer reviewed

Three-dimensional analysis of infiltration from the disc infiltrometer: 2. Physically based infiltration equation

R. Haverkamp, P.J. Ross, K.R.J. Smettem and J.Y. Parlange
Water Resources Research, Vol.30(11), pp.2931-2935
1994
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Abstract

In situ measurement of soil hydraulic properties may be achieved by analyzing the unconfined efflux from disc tension infiltrometers, once consistent infiltration equations can be derived. In this paper an analytical, three‐dimensional infiltration equation is developed, based on the use of parameters with sound physical meaning and adjustable for varying initial and boundary conditions. The equation is valid over the entire time range. For practical purposes, a simplified solution is also derived. The full and simplified equations give excellent agreement with published experimental results and are particularly useful for determining soil hydraulic properties through application of inverse procedures.

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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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