To obtain Cu-kaolinites with a controlled range of chemical compositio
ns, syntheses were performed by hydrothermally ageing gels with kaolin
ite stoichiometric compositions. Gels were prepared with sodium metasi
licate and nitrates of octahedral cations. Temperature of synthesis wa
s 250 degrees C with a corresponding equilibrium water pressure of 38
bars. Three samples with copper contents ranging from 0.1 to 7% and an
other one with the chemical composition of the Cu end-member were synt
hesized. While this fourth sample led to tenorite after the hydrotherm
al treatment, the three others crystallized well into kaolinite. Up to
almost 1% CuO was measured by TEM in some isolated 'clean' and hexago
nal kaolinite particles. EPR and XPS spectroscopies were consistent wi
th an octahedral position of Cu2+. In IR spectra, vAl-OH-Cu absorption
bands were not observed, but vAl(2)OH bands appeared more and more bl
urred when Cu content of samples increased. Weak bands situated at 868
cm(-1) and 840 cm(-1) are tentatively attributed to delta AlCuOH. By
differential thermal analysis, a downward shift of 20 degrees C in tem
perature of the endothermic peak from the less Cu-rich sample to the m
ost Cu-rich one, argued for the existence of some Al-OH-Cu bonds, whos
e binding energies are presumed to be less than the Al-OH-Al ones. In
view of these results, Cu2+ appears incorporated in the octahedral she
et of kaolinite. Moreover, this incorporation is made without major pe
rturbation of the kaolinite structure.