Changes produced after hydrothermal treatments at 400 OC and at different p
ressures in a set of Lu-saturated smectites have been compared with those o
ccurring in a mixture of 2SiO(2):1Lu(2)O(3). The effect of the mineralogica
l composition of the smectite on the reactivity has been analyzed. The grow
th of a new crystalline phase, Lu2Si2O7 (detected by means of X-ray diffrac
tion), at a different pressure for each smectite, has allowed us to establi
sh a reactivity order among the samples. All the samples were much more rea
ctive than the mixture of oxides. The reactivity of the smectites was modul
ated by their different mineralogical compositions. First, smectites having
Al in the tetrahedral sheet were the most reactive. This finding is interp
reted as due to a strong electrostatic interaction created by the Al that a
ctivates neighboring Si for the reaction. Second, a higher reactivity was o
bserved for the smectites with total occupancy of the octahedral sheet, due
to the simultaneous disruption of the tetrahedral-octahedral shared oxygen
layer and the diffusion of octahedral cations into the interlayer space. T
hird, the layer charge of the smectite does not induce any variation in the
reactivity for the set of samples analyzed.