The chemical, textural and structural transformations of Al-13-intercalated
montmorillonite, resulting from the depolymerization of the interlamellar
Al-13 polycations by Na salicylate solutions, were studied. Nitrogen gas ad
sorption shows a dramatic decrease in specific surface area from 493 to 39
m(2)g(-1), due to the loss of microporosity. Modelling of small-angle X-ray
scattering (SAXS) curves shows that the final product contains two phases:
a Na-exchanged swelling phase accounting for 40% of the clay, and a fixed
interlayer distance (20.8 Angstrom) phase accounting for 60% of the clay. T
he Al remaining in the clay galleries (45% of the initial Al) is composed o
f 13% Al-13 and 87% hexacoordinated At, probably Al(OH)(3)(0) and oligomeri
c Al-salicylate complexes, as shown by 27 Al NMR. The instability of Al-13-
intercalated montmorillonite towards organic ligands is related to the hydr
ation shell of the tridecamer, revealed by SAXS. These results focus on the
necessity to take into account the presence of organic ligands in natural
media when using materials such as Al-13-intercalated clays.