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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Formato: | article |
Lenguaje: | EN |
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Nature Portfolio
2017
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Acceso en línea: | https://doaj.org/article/8cec503ecc854d73890d18d5e80d998b |
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