Transport in Porous Media

, Volume 36, Issue 2, pp 211–244

Coupled Solvent and Heat Transport of a Mixture of Swelling Porous Particles and Fluids: Single Time-Scale Problem

  • Lynn Schreyer Bennethum
  • John H. Cushman

DOI: 10.1023/A:1006534302277

Cite this article as:
Bennethum, L.S. & Cushman, J.H. Transport in Porous Media (1999) 36: 211. doi:10.1023/A:1006534302277


A three-spatial scale, single time-scale model for both moisture and heat transport is developed for an unsaturated swelling porous media from first principles within a mixture theoretic framework. On the smallest (micro) scale, the system consists of macromolecules (clay particles, polymers, etc.) and a solvating liquid (vicinal fluid), each of which are viewed as individual phases or nonoverlapping continua occupying distinct regions of space and satisfying the classical field equations. These equations are homogenized forming overlaying continua on the intermediate (meso) scale via hybrid mixture theory (HMT). On the mesoscale the homogenized swelling particles consisting of the homogenized vicinal fluid and colloid are then mixed with two bulk phase fluids: the bulk solvent and its vapor. At this scale, there exists three nonoverlapping continua occupying distinct regions of space. On the largest (macro) scale the saturated homogenized particles, bulk liquid and vapor solvent, are again homogenized forming four overlaying continua: doubly homogenized vicinal fluid, doubly homogenized macromolecules, and singly homogenized bulk liquid and vapor phases. Two constitutive theories are developed, one at the mesoscale and the other at the macroscale. Both are developed via the Coleman and Noll method of exploiting the entropy inequality coupled with linearization about equilibrium. The macroscale constitutive theory does not rely upon the mesoscale theory as is common in other upscaling methods. The energy equation on either the mesoscale or macroscale generalizes de Vries classical theory of heat and moisture transport. The momentum balance allows for flow of fluid via volume fraction gradients, pressure gradients, external force fields, and temperature gradients.

swellingheat transferpolymerclayliquid/vapor transferdryingunsaturatedmixture.

Copyright information

© Kluwer Academic Publishers 1999

Authors and Affiliations

  • Lynn Schreyer Bennethum
    • 1
  • John H. Cushman
    • 2
  1. 1.Center for Computational MathematicsUniversity of Colorado at DenverDenverU.S.A
  2. 2.Center for Applied MathPurdue UniversityWest LafayetteU.S.A