The treatment of KGa-1 kaolinite with dimethyl sulfoxide and ammonium fluor
ide heated at 383 K provides an unstable hydrated phase characterized by a
10 Angstrom basal distance. When air-dried, this hydrate gives a dehydrated
phase at 7.15 Angstrom. The aim of this work is to determine the structura
l characteristics of this hydrate. The method used to characterize this hyd
rate is based on the comparison between experimental and calculated X-ray d
iffraction profiles. This study is achieved in two steps: the study of 00l
reflections enabled the determination of the number of intercalated water m
olecules, their positions and the stacking mode along the normal to the (a,
b) plane; and the study of the hkl reflections with h and/or k not equal 0
enabled the determination of the stacking mode and the positions of water
molecules in the (a, b) plane. The unstable hydrate is characterized by two
water molecules per Al2Si2O5(OH)(4) unit situated at z(1) = z(2) = 7.57 An
gstrom. Two adjacent layers are translated with respect to each other with
T-I = -0.155a + 0.13b + 10n.