2014
DOI: 10.1002/qua.24703
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Computer simulations of cations order‐disorder in 2:1 dioctahedral phyllosilicates using cation‐exchange potentials and monte carlo methods

Abstract: This article reviews the use of Monte Carlo methods with cation-exchange potentials and effective Hamiltonians, based on empirical potentials and quantum-mechanical calculations, for the study of cation ordering in phyllosilicates. The basic methodology is described, and the application of the methods is illustrated with a number of key example case studies. These include Al-Si ordering in muscovite, Al-Fe-Mg ordering (both binary and ternary compositions) in the octahedral illite/smectite sheet, examination o… Show more

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Cited by 10 publications
(10 citation statements)
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“…Thus, it is necessary to build a muscovite model with explicit arrangement of Al for comprehensive investigation of V substitution. The isomorphic substitutions in 2:1 dioctahedral phyllosilicates show a considerable short-range order but no long-range order [17,18]. Previous theoretical and experimental studies on muscovite found an ordered distribution of the cations in the T sheet with the Loewenstein Al-avoidance rule [19][20][21].…”
Section: Structure and Modelsmentioning
confidence: 99%
“…Thus, it is necessary to build a muscovite model with explicit arrangement of Al for comprehensive investigation of V substitution. The isomorphic substitutions in 2:1 dioctahedral phyllosilicates show a considerable short-range order but no long-range order [17,18]. Previous theoretical and experimental studies on muscovite found an ordered distribution of the cations in the T sheet with the Loewenstein Al-avoidance rule [19][20][21].…”
Section: Structure and Modelsmentioning
confidence: 99%
“…17−19 It was shown that Mg cations are preferentially dispersed, whereas Fe cations tend to form either clusters or chains. 19 Recently, Lavikainen and coworkers 20 used the density functional theory (DFT) approach to study the interaction of octahedral and tetrahedral charged substitutions in tv dioctahedral smectites. Accordingly, these substitutions tend to be dispersed in the layer structure.…”
Section: ■ Introductionmentioning
confidence: 99%
“…The regularity of the pillar alignment relies on nonbondinge lectrostatic repulsions between pillars and therefore ah omogeneous charged ensity is crucial.I nn aturalc lays like montmorillonite isomorphous substitution inevitably leads to segregation of different octahedral cations accompanied by chargeh eterogeneities and disables them as hosts for MOPS. [21] Only when increasing the impact of entropy in am elt synthesis [22] layered silicates with homogenous charge density suitable for MOPS are accessible.…”
Section: It'sa Ll About Functional Holes!mentioning
confidence: 99%