2006
DOI: 10.1039/b506932g
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On the application of computer simulation techniques to anionic and cationic clays: A materials chemistry perspective

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Cited by 129 publications
(132 citation statements)
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“…5 As a result of their high surface area and cation exchange properties, these minerals, whether from natural deposits or synthetic analogues, have found multiple practical applications and have been extensively studied using both analytical laboratory based techniques as well as molecular simulations. [6][7][8] The surfaces of both zeolite and clay minerals present an interesting contrast to silicate minerals as surface bound exposed cations possess a large enthalpy of hydration and (depending on the cation) present water wetting domains, where as the silicate domains behave more akin to quartz, with hydrophobic properties. 9 Though the clay minerals with large cation exchange capacity are of significant interest, they constitute a far smaller fraction of total soil mineral content relative to the alumi-3 nosilicate kaolinite minerals.…”
Section: Introductionmentioning
confidence: 99%
“…5 As a result of their high surface area and cation exchange properties, these minerals, whether from natural deposits or synthetic analogues, have found multiple practical applications and have been extensively studied using both analytical laboratory based techniques as well as molecular simulations. [6][7][8] The surfaces of both zeolite and clay minerals present an interesting contrast to silicate minerals as surface bound exposed cations possess a large enthalpy of hydration and (depending on the cation) present water wetting domains, where as the silicate domains behave more akin to quartz, with hydrophobic properties. 9 Though the clay minerals with large cation exchange capacity are of significant interest, they constitute a far smaller fraction of total soil mineral content relative to the alumi-3 nosilicate kaolinite minerals.…”
Section: Introductionmentioning
confidence: 99%
“…Indeed, classical MD is one of the key techniques used to model clay systems in the literature. 20,21 The main disadvantage of classical MD simulations is the lack of bond breaking and bond formation, hence chemical reactions are impossible to model using classical MD without specialist forcefields. 22 The aim of the present study is to model the effects of double layer expansion, multicomponent ionic exchange, and pH levels on the absorption of organic oil molecules on smectite clay basal surfaces as a function of salt concentration using atomistic MD.…”
Section: Introductionmentioning
confidence: 99%
“…1. Chemical structures of these clays have also been published by Itoh et al 2 ,a n dG r e e n w e l let al 3 , respectively. The layer surface has 0.25 to 1.2 negative charges per unit cell and a commensurate number of exchangeable cations in the interlamellar galleries.…”
Section: Introductionmentioning
confidence: 74%
“…37 reinforce, but rather to change the rheological behavior of the polyol solution during preparation of rigid PU foams. 141 Higher viscosity of the thixotropic system stabilized a dispersion of flame retardants [Sb 2 O 3 , Al(OH) 3 , CB, or melamine], while on shearing dramatically reduced viscosity facilitated foaming. The resulting hard PU foam had good dimensional stability and fire-resistance.…”
Section: Pnc With Lucentitementioning
confidence: 99%
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