However, the assumptions of small slope inherent in the diffusion-wave equation will not allow for modeling of inertial effects. 39,95 €Price includes VAT (Pakistan)Rent this article via DeepDyve. The two-component approach also enables the description of phase transition processes (evaporation, solution) under an equilibrium condition. Work with us. If you decide to access other
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Graf [2005] incorporated heat transport within the saturated-zone flow regime into HydroGeoSphere together with temperature-dependent fluid properties, such as viscosity and density. For each time step, the model solves surface and subsurface flow, solute and energy transport equations simultaneously, and provides a complete water and solute balance. 3 The code was further developed jointly at the University of Waterloo and the Laval University, and was primarily used for academic research. These Terms of Use are governed by the laws of the Province of Ontario
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Learn more. in repository systems) can be investigated numerically, including media dry-out and resaturation, consolidation, stress- or deformation-dependent permeabilities, thermal expansion and heat-induced stresses, gas transport processes in fully or partially saturated media and others.
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Correspondence to
Viacheslav Iegupov . The surface flow equation is solved on a 2-D finite-element mesh stacked upon a subsurface grid when solving for both domains (i. .