This paper extends the double porosity deformable model previously develope
d by one of the authors to include temperature effects. Unlike the double t
emperature approach, the model assumes a single representative thermodynami
cs continuum which includes both conduction and convection heat transfer in
a fully saturated porous media. Examples are presented to evaluate the sui
tability of the model. Copyright (C) 2000 John Wiley & Sons, Ltd.