WATER FLOW IN SOIL MACROPORES III. A STATISTICAL APPROACH

GERMANN, P. and BEVEN, K. (1981) WATER FLOW IN SOIL MACROPORES III. A STATISTICAL APPROACH. Journal of Soil Science, 32 (1). pp. 31-39. ISSN 0022-4588

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Abstract

Two regression equations describing water movement in saturated macropores in the field are compared with a theoretical expresion of the form Qmaα e2ma where Qma is the saturated volume flux density through a macropore system of porosity ema. The theoretical exponent of 2 agrees fairly well with the analyses of two very different sets of field experiments by Burger (1922–1940) and Ehlers (1975). It is suggested that the relationship Qma= Q*e2ma may be a useful first approximation to predict macropore flow, where Q* is an empirical coefficient that is expected to depend on the hydraulic connectivity, geometrical structure, tortuosity, roughness and other properties of the macropore system.

Item Type:
Journal Article
Journal or Publication Title:
Journal of Soil Science
Uncontrolled Keywords:
/dk/atira/pure/subjectarea/asjc/2300/2300
Subjects:
?? general environmental sciencesoil sciencegeneral agricultural and biological sciencesgeneral earth and planetary sciences ??
ID Code:
225028
Deposited By:
Deposited On:
15 Oct 2024 09:50
Refereed?:
Yes
Published?:
Published
Last Modified:
15 Oct 2024 09:50