A new three-dimensional numerical model of coupled heat, moisture and air transfer in unsaturated soil is presented. In particular, the model accommodates moisture transfer in the form of liquid and vapour flow and heat transfer arising from conduction, convection and latent heat of vaporization. Th
Three-dimensional coupled heat, moisture, and air transfer in a deformable unsaturated soil
β Scribed by H. R. Thomas; H. Missoum
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 233 KB
- Volume
- 44
- Category
- Article
- ISSN
- 0029-5981
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β¦ Synopsis
A three-dimensional numerical model is presented for three-phase flow (moisture, air, and heat) in a deformable partly saturated soil with deformation calculated via a non-linear elastic theory. The present work is an extension of a two-dimensional analysis presented by Thomas and He. The objective of this work is the solution of problems of greater geometric complexity. The mathematical formulation of this coupled problem consists of four governing equations, developed from the principles of mass and energy conservations as well as the stress equilibrium equation. Darcy's flow law is used to describe the motion of liquid and air in the porous medium, and a Philip and de Vries type vapour flow approach is employed in the formulation. A Galerkin finite element method coupled with a finite difference recurrence relationship is used to obtain simultaneous solutions to the governing equations where pore liquid, pore air pressures, temperature and displacements are the primary variables. The method allows the non-linear nature of the soil parameters to be modelled. Three-dimensional 20-noded isoparametric elements are used to simulate different types of cases for the verification of the work. Results are presented of the application of the new model to four problems, two of which are isothermal and two heating simulations. The three-dimensional nature of the results achieved is highlighted.
π SIMILAR VOLUMES
This paper presents a formulation for coupled heat and moisture transfer in a deformable partially saturated soil. The research is based on a mechanistic phase interaction model coupled to a state surface approach. The method takes into account the coupling effect of temperature gradient and deforma
A parallel numerical finite difference model, employing the self-implicit method, for coupled heat and moisture transfer in unsaturated soil is presented. The model is programmed in Occam and executed on a parallel computing network of transputers. An assessment of the model was achieved via the sim