Normally synthetic well defined monodisperse discotic laponite clays are kn
own to form a gel phase at mass concentrations as low as a few percent in d
istilled water. Hydrosoluble polymer polyethylene oxide was added to this i
ntriguing clay system, it was observed that it either prevents gelation or
slows it down extremely depending on the polymer weight, concentration or t
he laponite concentration. Small Angle Neutron scattering (SANS) was used t
o study these systems because only by isotopic labelling can the structure
of the adsorbed polymer layers be determined. The contrast variation techni
que is specifically used to determine separately the different partial stru
cture factors of the clay and polymer. In this way the signal of the adsorb
ed chains is separated from the signal of the free chains.