Modeling nonwetting-phase relative permeability accounting for a discontinuous nonwetting phase

被引:29
作者
Fischer, U
Dury, O
Fluhler, H
vanGenuchten, MT
机构
[1] ETH ZURICH, INST TERR ECOL, CH-8952 SCHLIEREN, SWITZERLAND
[2] ARS, US SALIN LAB, USDA, RIVERSIDE, CA 92507 USA
关键词
D O I
10.2136/sssaj1997.03615995006100050009x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
A model Par the wetting and nonwetting-phase constitutive relationships is presented. The nonwetting-phase relative permeability in the model is a function of the degree of continuous nonwetting-phase saturation. Different formulations of the continuous nonwetting-phase model were evaluated by comparison of calculated anti measured air permeabilities as well as discontinuous air saturations. A Brooks and Corey-Burdine type formulation of the nonwetting phase relative permeability was more accurate than the corresponding van Genuchten-Mualem equation. Estimated discontinuous air saturations were higher for drying than for wetting, thus reflecting hysteresis in the water-retention smd relative air permeability functions. The continuous nonwetting-phase model provided a much better prediction of relative air permeabilities than a formulation that neglects the presence of a discontinuous nonwetting phase. Three emergence point model for the nonwetting-phase relative permeability provided a good approximation of the continuous nonwetting-phase model.
引用
收藏
页码:1348 / 1354
页数:7
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