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The Exchange Mechanism of Alkaline and Alkaline-Earth Ions in Zeolite N

Zeolite N is a synthetic zeolite of the EDI framework family from the more than 200 known zeolite types. Previous experimental laboratory and field data show that zeolite N has a high capacity for exchange of ions. Computational modelling and simulation techniques are effective tools that help expla...

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Detalles Bibliográficos
Autores principales: Khosravi, Monireh, Murthy, Vinuthaa, D R Mackinnon, Ian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6832695/
https://www.ncbi.nlm.nih.gov/pubmed/31658670
http://dx.doi.org/10.3390/molecules24203652
Descripción
Sumario:Zeolite N is a synthetic zeolite of the EDI framework family from the more than 200 known zeolite types. Previous experimental laboratory and field data show that zeolite N has a high capacity for exchange of ions. Computational modelling and simulation techniques are effective tools that help explain the atomic-scale behaviour of zeolites under different processing conditions and allow comparison with experiment. In this study, the ion exchange behaviour of synthetic zeolite N in an aqueous environment is investigated by molecular dynamics simulations. The exchange mechanism of K(+) extra-framework cations with alkaline and alkaline-earth cations NH(4)(+), Li(+), Na(+), Rb(+), Cs(+), Mg(2+) and Ca(2+) is explored in different crystallographic directions inside the zeolite N structure. Moreover, the effect of different framework partial charges on MD simulation results obtained from different DFT calculations are examined. The results show that the diffusion and exchange of cations in zeolite N are affected by shape and size of channels controlling the ion exchange flow as well as the nature of cation, ionic size and charge density.