The thermodynamic properties of the hydration water of hydrated minerals co
ntribute to the variations of the solubility products and cation selectivit
y constants. This is illustrated here as an example taken from series of hy
drated magnesium and strontium chlorides. Such variations are a function of
temperature, pressure, or activity of water. The proposed method, applicab
le to clay minerals, allows hydration processes to be taken into account fo
r calculating solubility products when only the thermodynamic properties ei
ther of the dehydrated or hydrated mineral phase, the hydration isotherm of
the mineral and the thermodynamic properties of the hydration water are es
tablished. (C) 2000 Academie des sciences / Editions scientifiques et medic
ales Elsevier SAS.