2018
DOI: 10.3390/min8050205
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Classical Polarizable Force Field to Study Hydrated Hectorite: Optimization on DFT Calculations and Validation against XRD Data

Abstract: Following our previous works on dioctahedral clays, we extend the classical Polarizable Ion Model (PIM) to trioctahedral clays, by considering dry Na-, Cs-, Ca- and Sr-hectorites as well as hydrated Na-hectorite. The parameters of the force field are determined by optimizing the atomic forces and dipoles on density functional theory calculations. The simulation results are validated by comparison with experimental X-ray diffraction (XRD) data. The XRD patterns calculated from classical molecular dynamics simul… Show more

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Cited by 12 publications
(18 citation statements)
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“…However, PIM has already shown a very good agreement with the experiments on the structure of concentrated solutions 47,89 as well as on the structure of clays. [48][49][50][51] We can thus assume that PIM may correctly describe the structure of the species at the interface. To test this assumption, it would be interesting to reproduce this study on clays more tractable experimentally, such as muscovites, on which reflectivity studies can be conducted.…”
Section: Resultsmentioning
confidence: 99%
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“…However, PIM has already shown a very good agreement with the experiments on the structure of concentrated solutions 47,89 as well as on the structure of clays. [48][49][50][51] We can thus assume that PIM may correctly describe the structure of the species at the interface. To test this assumption, it would be interesting to reproduce this study on clays more tractable experimentally, such as muscovites, on which reflectivity studies can be conducted.…”
Section: Resultsmentioning
confidence: 99%
“…PIM was developed initially for the modeling of aqueous electrolytes, 47 and was extended more recently to include the parameters necessary to model various clay minerals and zeolites. [48][49][50][51] In this force field each atom is treated as a polarizable charged ball.…”
Section: Molecular Dynamics Force Fieldsmentioning
confidence: 99%
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“…H-bonding plays a crucial role in their properties, either in their interactions with water 17,[22][23][24][25] or, in the case of so-called 1:1 clays whose layers comprise an H-bond donating and an H-bond accepting sheet, in the cohesive forces holding these layers together 13,26,27 . Theoretical studies have been carried out at multiple scales, from quantum-mechanical calculations intended to find the ground-state structure of clays and characterize the types of H-bonding [27][28][29][30][31][32] to molecular dynamics simulations, either using ab initio descriptions of the electron structure to study clay wetting 14,24 or acidbase chemistry 33,34 or larger-scale studies with classical forcefields 26,35 to model diffraction 36 or vibrational spectroscopy 37 experiments.…”
Section: Introductionmentioning
confidence: 99%
“…H-bonding plays a crucial role in their properties, either in their interactions with water 17,[22][23][24][25] or, in the case of so-called 1:1 clays whose layers comprise an H-bond donating and an H-bond accepting sheet, in the cohesive forces holding these layers together 13,26,27 . Theoretical studies have been carried out at multiple scales, from quantum-mechanical calculations intended to find the ground-state structure of clays and characterize the types of H-bonding [27][28][29][30][31][32] to molecular dynamics simulations, either using ab initio descriptions of the electron structure to study clay wetting 14,24 or acidbase chemistry 33,34 or larger-scale studies with classical forcefields 26,35 to model diffraction 36 or vibrational spectroscopy 37 experiments.…”
Section: Introductionmentioning
confidence: 99%