  In this work stability of Laponite against dissolution in its aqueous
dispersions is investigated as a function of initial pH of water before mixing
Laponite, and concentration of Laponite. Dissolution of Laponite is quantified
in terms of concentration of leached magnesium in the dispersions.
Interestingly the solvent pH is observed to play no role in dissolution of
Laponite in dispersion over the explored range of 3 to 10. Furthermore,
contrary to the usual belief that Laponite dissolves when pH of aqueous
dispersion decreases below 9, dissolution of the same is observed even though
dispersion pH is above 10 for low concentrations of Laponite (1 and 1.7 mass%).
On the other hand, for dispersions having high concentration of Laponite (2.8
mass%) and pH in the similar range (>10) no dissolution is observed.
Measurement of ionic conductivity of dispersion shows that concentration of
sodium ions in dispersion increases with concentration of Laponite, which
appears to have a role in preventing the dissolution of Laponite.
