Clays and Clay Minerals · 1990 · 54 citations · 9 references
AgricultureChemistrySoil SciencesMineralogySoil-water RelationsWater TreatmentCation Exchange CapacityClay DispersionClay MineralogyMoisture SorptionClay Mineral SwellingClay Swelling BehaviorSwelling
Abstract The swelling of an n-butylammonium vermiculite in solutions of n-butylammonium chloride has been studied by neutron diffraction as a function of temperature and the concentration of the soaking solution. On heating a swollen sample a transition to the crystalline phase took place at a well-defined temperature, the c -axis spacing changing from 120 to 19.4 Å at 14°C in a 0.1 M solution and from 330 to 19.4 Å at 33°C in a 0.01 M solution. The phase transition was completely reversible, and a study of the temperature-concentration phase diagram was made as high as 50°C The swollen phase was studied in a range of concentrations of the external solution between 0.2 M and 5 × 10 -4 M, for which the c -axis spacings were 85 and 910 Å, respectively. The reversibility, sharpness, and reproducibility of the phase change from crystalline to swollen gel suggest that the transition is truly thermodynamic, which is not in accord with DLVO theory. The concentration dependence of the observed d-values also could not be explained satisfactorily by DLVO theory.
9
The London—van der Waals attraction between spherical particles
H. C. Hamaker · Physica · 1937 · 3.9K citations
An Introduction to Clay Colloid Chemistry
H. van Olphen · Soil Science · 1964 · 2.6K citations