Please use this identifier to cite or link to this item: http://hdl.handle.net/10125/30478

Two-domain estimation of hydraulic properties in macropore soils

Item Summary

dc.contributor.author Chen, Chuan
dc.contributor.author Thomas, Donald M.
dc.contributor.author Green, Richard E.
dc.contributor.author Wagenet, Robert Jeffrey
dc.date.accessioned 2013-09-06T23:15:52Z
dc.date.available 2013-09-06T23:15:52Z
dc.date.issued 1993-05/1993-06
dc.identifier.citation Soil Science Society of America Journal. May-June 1993. Two-Domain Estimation of Hydraulic Properties in Macropore Soils. Madison, WI: Soil Science Society of America Journal.
dc.identifier.uri http://hdl.handle.net/10125/30478
dc.description.abstract Estimation of hydraulic: properties or soils having macropores is difficult, yet very important for describing soil-water flow dynamics. Conventional approaches of defining macroporosity based on pore size may not be generally successful quantitatively relating macroporosity to the dynamics of water flow. A definition or macroporosity based on water flux at different degrees or water saturation can be expected to be more useful. This study attempted to quantify the functional macroporosity of field soil from In situ measurements of water content, 6 (z, t), during drainage of an initially field-saturated soil. The soil was assumed to be a two-domain water flow system comprised of macropores, which dominate the early drainage process, and the matrix pore space, which is responsible for drainage occurring after macropores are emptied. The unit hydraulic gradient approach of calculating hydraulic productivity was extended and applied to the two-domain system. Field-measured data for a well-drained Wahiawa soil (clayey, kaolinitic, isohyperthermic Tropeptic Eutrustox) in Hawaii are used to test the approach. The partitioned hydraulic conductivities obtained for the two domains appeared qualitatively realistic, and when summed, resulted in a composite saturated conductivity which was close to that measured by the in situ instantaneous profile method. In addition, the macosporosites obtained from drainage calculations for three soil depths were very similar to those obtained from water retention measurements on undisturbed soil cores from the same field site. The proposed approach thus appears to be a promising method for evaluating hydraulic properties for a well-drained soil profile containing macrospores.
dc.format.extent 7 pages
dc.language.iso en-US
dc.publisher Soil Science Society of America Journal
dc.subject radon
dc.subject fluid flow
dc.subject journal articles
dc.title Two-domain estimation of hydraulic properties in macropore soils
dc.type Journal Article
dc.type.dcmi Text
Appears in Collections: HIGP Miscellaneous Documents
The Geothermal Collection


Please email libraryada-l@lists.hawaii.edu if you need this content in ADA-compliant format.

Items in ScholarSpace are protected by copyright, with all rights reserved, unless otherwise indicated.