Open AccessMulti-phase reactive transport theory
Author(s) -
Peter C. Lichtner
Publication year - 1995
Language(s) - English
Resource type - Reports
DOI - 10.2172/95551
Subject(s) - porous medium , thermodynamics , porosity , permeability (electromagnetism) , capillary action , chemistry , wetting , dissolution , fick's laws of diffusion , mechanics , diffusion , physics , biochemistry , organic chemistry , membrane
Physicochemical processes in the near-field region of a high-level waste repository may involve a diverse set of phenomena including flow of liquid and gas, gaseous diffusion, and chemical reaction of the host rock with aqueous solutions at elevated temperatures. This report develops some of the formalism for describing simultaneous multicomponent solute and heat transport in a two-phase system for partially saturated porous media. Diffusion of gaseous species is described using the Dusty Gas Model which provides for simultaneous Knudsen and Fickian diffusion in addition to Darcy flow. A new form of the Dusty Gas Model equations is derived for binary diffusion which separates the total diffusive flux into segregative and nonsegregative components. Migration of a wetting front is analyzed using the quasi-stationary state approximation to the Richards` equation. Heat-pipe phenomena are investigated for both gravity- and capillary-driven reflux of liquid water. An expression for the burnout permeability is derived for a gravity-driven heat-pipe. Finally an estimate is given for the change in porosity and permeability due to mineral dissolution which could occur in the region of condensate formation in a heat-pipe