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Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores

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Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores. / Germann, Peter F.; Beven, Keith.
In: Water Resources Research, Vol. 21, No. 7, 07.1985, p. 990-996.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

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Germann PF, Beven K. Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores. Water Resources Research. 1985 Jul;21(7):990-996. doi: 10.1029/WR021i007p00990

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Germann, Peter F. ; Beven, Keith. / Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores. In: Water Resources Research. 1985 ; Vol. 21, No. 7. pp. 990-996.

Bibtex

@article{2a5d70f317824657b3ece954edc2cb44,
title = "Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores",
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.",
author = "Germann, {Peter F.} and Keith Beven",
year = "1985",
month = jul,
doi = "10.1029/WR021i007p00990",
language = "English",
volume = "21",
pages = "990--996",
journal = "Water Resources Research",
issn = "0043-1397",
publisher = "AMER GEOPHYSICAL UNION",
number = "7",

}

RIS

TY - JOUR

T1 - Kinematic Wave Approximation to Infiltration Into Soils With Sorbing Macropores

AU - Germann, Peter F.

AU - Beven, Keith

PY - 1985/7

Y1 - 1985/7

N2 - 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.

AB - 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.

UR - http://www.scopus.com/inward/record.url?scp=0022101913&partnerID=8YFLogxK

U2 - 10.1029/WR021i007p00990

DO - 10.1029/WR021i007p00990

M3 - Journal article

AN - SCOPUS:0022101913

VL - 21

SP - 990

EP - 996

JO - Water Resources Research

JF - Water Resources Research

SN - 0043-1397

IS - 7

ER -