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Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores

Peter Germann, Keith Beven

Open publisher page 234 citations

Abstract

Infiltration into soils with macropores is treated as two‐domain flow. The first domain is the soil matrix, in which water is subjected to capillarity, and infiltration is approached by Philip's sorptivity concept. The second domain is the soil macropore system in which water moves only under gravity and flow is approached by kinematic wave theory. A sink function with respect to flow in the macropore system accounts for water sorption by the soil matrix. The two‐domain flow model is then applied to infiltration into a block of undisturbed soil containing macropores.

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Infiltration into soils with macropores is treated as two‐domain flow. The first domain is the soil matrix, in which water is subjected to capillarity, and infiltration is approached by Philip's sorptivity concept. The second domain is the soil macropore system in which water moves only under gravity and flow is approached by kinematic wave theory. A sink function with respect to flow in the macropore system accounts for water sorption by the soil matrix. The two‐domain flow model is then applied to infiltration into a block of undisturbed soil containing macropores.

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Available abstract

Infiltration into soils with macropores is treated as two‐domain flow. The first domain is the soil matrix, in which water is subjected to capillarity, and infiltration is approached by Philip's sorptivity concept. The second domain is the soil macropore system in which water moves only under gravity and flow is approached by kinematic wave theory. A sink function with respect to flow in the macropore system accounts for water sorption by the soil matrix. The two‐domain flow model is then applied to infiltration into a block of undisturbed soil containing macropores.

Key concepts: Macropore, Sorptivity, Infiltration (HVAC), Kinematic wave, Soil water, Soil science, Sorption, Characterisation of pore space in soil

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