Different route of hydroxide incorporation and thermal stability of new type of water clathrate: X-ray single crystal and Raman investigation

Abstract Chlormayenite Ca12Al14O32[♦4Cl2] (♦-vacancy) is partially hydrated micro porouss mineral with hydroxide groups situated at various crystallographic sites. There are few mechanisms describing its hydration. The first one assumes Cl− substitution by OH− at the center of the structural cages (...

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Autores principales: Mateusz Dulski, Katarzyna M. Marzec, Joachim Kusz, Irina Galuskina, Katarzyna Majzner, Evgeny Galuskin
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/8cec503ecc854d73890d18d5e80d998b
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