1981
DOI: 10.2172/6149346
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Studies of heat transfer and water migration in soils. Final report

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Cited by 26 publications
(3 citation statements)
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“…The combination of the Richards equation and conduction-convection heat equation as the governing model represents the water and heat transfer in soil. Such a model formulation does not include temperature gradient as a factor in the flux vapor transfer and associated sensible and latent heat fluxes; it may produce undesirable results in unsaturated soils [39]. Another limitation of Richard's equation in hygrothermal modeling is that it does not include the vapor phase of liquid.…”
Section: A Brief History Of Hygrothermal Modelsmentioning
confidence: 99%
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“…The combination of the Richards equation and conduction-convection heat equation as the governing model represents the water and heat transfer in soil. Such a model formulation does not include temperature gradient as a factor in the flux vapor transfer and associated sensible and latent heat fluxes; it may produce undesirable results in unsaturated soils [39]. Another limitation of Richard's equation in hygrothermal modeling is that it does not include the vapor phase of liquid.…”
Section: A Brief History Of Hygrothermal Modelsmentioning
confidence: 99%
“…latent heat fluxes; it may produce undesirable results in unsaturated soils [39]. Another limitation of Richard's equation in hygrothermal modeling is that it does not include the vapor phase of liquid.…”
Section: A Brief History Of Hygrothermal Modelsmentioning
confidence: 99%
“…Equation Description Temperature dependence of gas diffusion coefficients (Vargaftik, 1975;Walker et al, 1981)…”
Section: Eqn Nomentioning
confidence: 99%