Organoclay rheological type

Organoclay rheological type is defined by its unique flow and deformation properties, shaped by key characteristics inherited and modified from bentonite.

One aspect is its strong binding capacity: fine organoclay particles, with a large specific surface area (up to 800 m²/g) and high surface energy, form water film bridges and van der Waals forces between particles after adsorbing water, contributing to the rheological behavior that supports cohesion in various systems.

Its high plasticity index, allowing it to be shaped into various forms when mixed with water and retain shape after drying, further defines its rheological type. Adsorption capacity, both physical (for organics, pigments) and chemical via ion exchange, influences how the rheological type interacts with different media.

Organoclay rheological type:Thermal stability also plays a role—while losing adsorbed and interlayer water at 100 – 300°C causes volume shrinkage, modified rheological types like those based on sodium – bentonite maintain better performance at high temperatures, affecting their application range.