Abstract

AbstractThe swelling and cation exchange properties of montmorillonite are fundamental in a wide range of applications ranging from nanocomposites to catalytic cracking of hydrocarbons. The swelling results from several factors and, though widely studied, information on the effects of a single factor at a time is lacking. In this study, density functional theory (DFT) calculations were used to obtain atomic-level information on the swelling of montmorillonite. Molecular dynamics (MD) was used to investigate the swelling properties of montmorillonites with different layer charges and interlayer cationic compositions. Molecular dynamics calculations, with CLAYFF force field, consider three layer charges (−1.0, −0.66 and −0.5 e per unit cell) arising from octahedral substitutions and interlayer counterions of Na, K and Ca. The swelling curves obtained showed that smaller layer charge results in greater swelling but the type of the interlayer cation also has an effect. The DFT calculations were also seen to predict larger d values than MD. The formation of 1, 2 and 3 water molecular layers in the interlayer spaces was observed. Finally, the data from MD calculations were used to predict the selfdiffusion coefficients of interlayer water and cations in different montmorillonites and in general the coefficient increased with increasing water content and with decreasing layer charge.

Highlights

  • Smectites are 2:1 layered swelling clay minerals consisting of layers formed of two tetrahedral silicate sheets one on either side of an octahedral aluminium sheet

  • The Quantum mechanics (QM) and molecular dynamics (MD) simulations in the present study indicated that the interlayer water molecules form hydrogen bonds with the nearest cations and the oxygen atoms of the tetrahedral sheets

  • The present study indicated that both QM and MD can be used to study the crystalline swelling of montmorillonites

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Summary

Montmorillonite structure

The basic montmorillonite building unit is a 2:1 layer with an octahedral (O) sheet sandwiched between two tetrahedral (T) sheets (Viani et al, 2002). The TOT layers have a characteristic repeat distance and carry a net negative charge. The general unit-cell formula for Mgsubstituted montmorillonite where the substitutions, i.e. where M is an alkali or alkali earth exchangeable cation (Na+, K+ or Ca2) and x = 0.4 –1.2. Because the number of charge sites in the tetrahedral sheet is small compared to the number of sites in the octahedral sheet (Rowe et al, 1997), tetrahedral substitutions were not included in our small-scale calculations. The structure has a C2/m symmetry, and experimental lattice parameters are a = 518 pm, b = 897 pm, c = 995 pm, α = γ = 90.0° and β = 99.5° without water molecules in the interlayer space between the TOT layers

Quantum mechanics
Molecular dynamics
Effect of water on the structures
Hydration of cations
Interlayer structures
Diffusion of water and cations
CONCLUSIONS
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