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Theoretical Basis for Describing Thermally Induced Water Flux in Soils
This paper proposed a theory to address the underestimation of water flux by the model of Philip and de Vries for conditions without ice lenses. Experiments with a modified capillary rise method were proposed to calculate a gain factor, which accounts for this underestimation. For the thermally induced flux in frozen soils with ice lenses, a theoretical formulation was derived for the segregation potential, which is the key parameter in the model of Konrad and Morgenstern. This theoretical formulation, which is a unique contribution of this paper, is expressed in a simple mathematical form and can be conveniently used for accurate prediction of segregation potential.
Theoretical Basis for Describing Thermally Induced Water Flux in Soils
This paper proposed a theory to address the underestimation of water flux by the model of Philip and de Vries for conditions without ice lenses. Experiments with a modified capillary rise method were proposed to calculate a gain factor, which accounts for this underestimation. For the thermally induced flux in frozen soils with ice lenses, a theoretical formulation was derived for the segregation potential, which is the key parameter in the model of Konrad and Morgenstern. This theoretical formulation, which is a unique contribution of this paper, is expressed in a simple mathematical form and can be conveniently used for accurate prediction of segregation potential.
Theoretical Basis for Describing Thermally Induced Water Flux in Soils
Liu, Zhen (Autor:in) / Zhang, Bin (Autor:in) / Yu, Xiong (Autor:in)
Geo-Congress 2014 ; 2014 ; Atlanta, Georgia
Geo-Congress 2014 Technical Papers ; 3487-3495
24.02.2014
Aufsatz (Konferenz)
Elektronische Ressource
Englisch
Theoretical Basis for Describing Thermally Induced Water Flux in Soils
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