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Being able to understand the chemistry of the porewater in compacted bentonite is very important since it is critical to predicting radionuclide solubilities and to the synthesis of sorption data bases, and hence to repository safety studies.
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Bentonite fining is very common in white wines, where excessive grape proteins result in unsightly hazes.
Bentonite swelling is very sensitive to the pore solution concentration because increasing concentration suppresses the diffuse double layer component of swelling.
Bentonite is a very important naturally occurring clay and it is used in many great commercial processes.
Hydrated bentonite is a very plastic material and it is expected to enter in the rock microfractures at the granite/bentonite boundary of a deep geological high-level waste repository.
For these reasons, a textural characterization of bentonites in the laboratory is very important.
The proposed analytical model is very useful for understanding the influencing parameters on the bentonite behavior.
The swelling prediction of bentonite sand mixtures due to wetting is very important in evaluating the long term performance of the engineered barrier in the high level radioactive waste disposal system and the hydraulic barriers in geoenvironmental constructions.
However, changes of the effective porosity caused by bentonite swelling can be very large.
Bentonite is an active clay mineral with very low hydraulic conductivity and extremely high expansive properties, which benefits in controlling the downward migration of hazardous contaminants to groundwater.
The rheological properties of bentonite were characterized from very low strain rate to relatively high strain rate to determine the nonlinear behavior of the shear thinning drilling mud.
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