ON THE H-FORM OF NATROLITE

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dc.contributor.author Likhacheva A.Yu.
dc.contributor.author Belitsky I.A.
dc.contributor.author Veniaminov S.A.
dc.contributor.author Paukshtis E.A.
dc.date.accessioned 2024-07-14T10:19:05Z
dc.date.available 2024-07-14T10:19:05Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=13506356
dc.identifier.citation European Journal of Mineralogy, 2006, 18, 3, 345-350
dc.identifier.issn 0935-1221
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44419
dc.description.abstract To resolve the problem of existence of the H-form of natrolite, the thermal decomposition of NH4-exchanged natrolite (as a precursor of the H-form) was studied by gas chromatography, IR spectroscopy and X-ray diffraction. Throughout the decomposition, the de-ammoniation is immediately followed by dehydroxylation, which is evidence for the instability of the H-natrolite formed after the removal of NH3, and leads to a negligibly small concentration of the OH-groups. The natrolite structure can not persist after the removal of NH3. In the final step of decomposition, the adsorption of NH3 onto Lewis centres accumulated in the amorphosed framework hinders the de-ammoniation. This seems to be one of the major factors which influence the observed increase in the activation energy for NH3 desorption from 117 (± 13) kJ/mol in the initial step to 270 (±20) kJ/mol. Smooth vacuum degassing of NH4-natrolite at 550 K leads to partia l de-ammoniation, rather than formation of H-natrolite. © 2006 E. Schweizerbart'sche Verlagsbuchhandlung.
dc.subject AMMONIUM NATROLITE
dc.subject AMORPHISATION
dc.subject DE-AMMONIATION
dc.subject DEHYDROXYLATION
dc.subject GAS CHROMATOGRAPHY
dc.subject H-NATROLITE
dc.subject IR SPECTROSCOPY
dc.subject NATROLITE
dc.title ON THE H-FORM OF NATROLITE
dc.type Статья
dc.identifier.doi 10.1127/0935-1221/2006/0018-0345


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