The surface properties of six clay samples (three illites and three ka
olinites formed under different logical conditions) were evaluated by
inverse gas chromatography at finite concentration conditions. The det
ermination of the adsorption isotherms for several organic probes, hex
ane, benzene, pyridine, and 2-propanol, on these clays allows the esti
mation of their energetic surface heterogeneity through the determinat
ion of their adsorption energy distribution functions. It was then sho
wn that, when the organic probe is well chosen, this method allows dis
tinguishing between the family of clay, illite or kaolinite, and even,
in a same family, between the different geological formation conditio
ns. The illite samples are more heterogeneous than the kaolinite sampl
es.