The desorption profiles of various organics from soil and activated ca
rbon using dense liquid and supercritical carbon dioxide were modeled.
The model accounts for effective diffusion of the organics in the sol
id pores, axial dispersion in the fluid phase, and external mass trans
fer to the fluid phase from the particle surface. This model, involvin
g partial differential equations, is solved using the orthogonal collo
cation on finite elements. The model is able to predict the experiment
al data quite well without any adjustable parameters. The importance o
f each parameter depended on the system, although adsorption equilibri
um and the effective pore diffusion of the organic were the most signi
ficant parameters in all the systems investigated.