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WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH

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WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH. / GERMANN, P.; BEVEN, K.
In: Journal of Soil Science, Vol. 32, No. 1, 03.1981, p. 1-13.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

GERMANN, P & BEVEN, K 1981, 'WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH', Journal of Soil Science, vol. 32, no. 1, pp. 1-13. https://doi.org/10.1111/j.1365-2389.1981.tb01681.x

APA

GERMANN, P., & BEVEN, K. (1981). WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH. Journal of Soil Science, 32(1), 1-13. https://doi.org/10.1111/j.1365-2389.1981.tb01681.x

Vancouver

GERMANN P, BEVEN K. WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH. Journal of Soil Science. 1981 Mar;32(1):1-13. doi: 10.1111/j.1365-2389.1981.tb01681.x

Author

GERMANN, P. ; BEVEN, K. / WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH. In: Journal of Soil Science. 1981 ; Vol. 32, No. 1. pp. 1-13.

Bibtex

@article{3be61ce5524e4bf4bede8198f6b7c423,
title = "WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH",
abstract = "A method is proposed by which the volume of the macropore system and its effect on the infiltration capacity can be estimated using a soil water potential concept. The macropore systems of two large and undisturbed soil samples were investigated. The volumes of macropores were 0.01 and 0.045 of the sample volumes, respectively. When the samples were drained from full saturation to the point where it may be assumed that there was no more water in the macropore system, the hydraulic conductivity decreased by factors of 18 and 4.3 respectively.",
author = "P. GERMANN and K. BEVEN",
year = "1981",
month = mar,
doi = "10.1111/j.1365-2389.1981.tb01681.x",
language = "English",
volume = "32",
pages = "1--13",
journal = "Journal of Soil Science",
issn = "0022-4588",
publisher = "Wiley-Blackwell",
number = "1",

}

RIS

TY - JOUR

T1 - WATER FLOW IN SOIL MACROPORES I. AN EXPERIMENTAL APPROACH

AU - GERMANN, P.

AU - BEVEN, K.

PY - 1981/3

Y1 - 1981/3

N2 - A method is proposed by which the volume of the macropore system and its effect on the infiltration capacity can be estimated using a soil water potential concept. The macropore systems of two large and undisturbed soil samples were investigated. The volumes of macropores were 0.01 and 0.045 of the sample volumes, respectively. When the samples were drained from full saturation to the point where it may be assumed that there was no more water in the macropore system, the hydraulic conductivity decreased by factors of 18 and 4.3 respectively.

AB - A method is proposed by which the volume of the macropore system and its effect on the infiltration capacity can be estimated using a soil water potential concept. The macropore systems of two large and undisturbed soil samples were investigated. The volumes of macropores were 0.01 and 0.045 of the sample volumes, respectively. When the samples were drained from full saturation to the point where it may be assumed that there was no more water in the macropore system, the hydraulic conductivity decreased by factors of 18 and 4.3 respectively.

UR - http://www.scopus.com/inward/record.url?scp=0019367248&partnerID=8YFLogxK

U2 - 10.1111/j.1365-2389.1981.tb01681.x

DO - 10.1111/j.1365-2389.1981.tb01681.x

M3 - Journal article

AN - SCOPUS:0019367248

VL - 32

SP - 1

EP - 13

JO - Journal of Soil Science

JF - Journal of Soil Science

SN - 0022-4588

IS - 1

ER -