This chapter investigates the phase diagram of extensively aged MMT dispersions. Formation of gel through different routes is reported. Distinctive phase separation, equilibrium fluid and equilibrium gels in the t w -c phase space are observed for the first time ever in MMT dispersions ( Fig. 5.1).
IntroductionPhase stability of dispersions of anisotropic particles has been of much scientific debate in the recent times. Many phase diagrams have been conceived and proposed for colloidal particles having different degree of geometrical anisotropy, namely rods, platelets, disks etc. in their dispersion states [2,28,29]. Spherical colloidal particles have been studied extensively in the literature. Clays are discotic platelets with varying aspect ratio and surface charge density. Because of this clay dispersions have exhibited non-trivial and rich phase diagrams, which have attracted much attention in recent years. Suspensions of clays have unique properties, including the ability to form arrested states like gels, glasses and liquid crystalline structures under ambient conditions as function of aging time and solid concentration. Remarkably, compared to spherical colloids, clay platelets exhibit gel and glass phases at very low concentrations which owe their origin to their structure and surface charge heterogeneity.Montmorillonite (MMT) is one of the natural clays, which has high aspect ratio and is a macroscopically swelling, 'active' clay that has the capacity for taking up large amounts of water to form stable gels. The phase diagram of MMT is least explored in the literature, though some attempts in that direction have been made in the past Michot et al. [16]. Michot et al. [16] studied the phase diagram of MMT using different aspect ratio samples. Recently, we have reported the sol and gel transition behavior of laponite-MMT mixed clay dispersions [21]. On the other hand, visco-elastic properties of MMT suspensions have extensively reported [4,8,17,22,25,26]. For instance, rheology behaviour of bentonite slurries as a function of pH, molar ratio of Na + /Ca +2 and with a range of additives such as pyrophosphate, polyphosphate [31]