Molecular scale understanding
of the structure and properties of
aqueous interfaces with clays, metal (oxy-) hydroxides, layered double
hydroxides, and other inorganic phases is strongly affected by significant
degrees of structural and compositional disorder of the interfaces.
ClayFF was originally developed as a robust and flexible force field
for classical molecular simulations of such systems (Cygan, R. T.;
Liang, J.-J.; Kalinichev, A. G. J. Phys. Chem. B
2004, 108, 1255–1266). However, despite its success,
multiple limitations have also become evident with its use. One of
the most important limitations is the difficulty to accurately model
the edges of finite size nanoparticles or pores rather than infinitely
layered periodic structures. Here we propose a systematic approach
to solve this problem by developing specific metal–O–H
(M–O–H) bending terms for ClayFF, E
bend
= k (θ – θ0)2 to better describe the structure and dynamics
of singly protonated hydroxyl groups at mineral surfaces, particularly
edge surfaces. On the basis of a series of DFT calculations, the optimal
values of the Al–O–H and Mg–O–H parameters
for Al and Mg in octahedral coordination are determined to be θ0,AlOH = θ0,MgOH = 110°, k
AlOH = 15 kcal mol–1 rad–2 and k
MgOH
= 6 kcal mol–1 rad–2. Molecular dynamics simulations were performed for
fully hydrated
models of the basal and edge surfaces of gibbsite, Al(OH)3, and brucite, Mg(OH)2, at the DFT level of theory and
at the classical level, using ClayFF with and without the M–O–H term. The addition
of the new
bending term leads to a much more accurate representation of the orientation
of O–H groups at the basal and edge surfaces. The previously
observed unrealistic desorption of OH2 groups from the
particle edges within the original ClayFF model is also strongly constrained
by the new modification.
Toward the development of classical force fields for the accurate modeling of clay mineral-water systems, we have extended the use of metal-O-H (M-O-H) angle bending terms to describe surface Si-O-H bending for hydrated kaolinite edge structures. Kaolinite, comprised of linked octahedral Al and tetrahedral Si sheets, provides a rigorous test by combining aluminol and silanol groups with water molecules in hydrated edge structures. Periodic density functional theory and classical force fields were used with molecular dynamics to evaluate structure, dynamics, hydrogen bonding, and power spectra for deriving optimum bending force constants and optimal equilibrium angles. Cleavage energies derived from density functional theory molecular dynamics (DFT-MD) calculations indicate the relative stability of both AC1 and AC2 edge terminations of kaolinite where Si-OH and Al-(OH2) or Si-OH, Al-OH, and Al-(OH2) groups exist, respectively. Although not examined in this study, the new Si-O-H angle bending parameter should allow for improved modeling of hydroxylated surfaces of silica minerals such as quartz and cristobalite, as well as amorphous silica-based surfaces and potentially those of other silicate and aluminosilicate phases.
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