LOCAL ORDER OF THE TRANSITION METALS FOR THE SUBSTITUTION COPPER-ALUMINUM-LAYERED DOUBLE HYDROXIDE-LIKE PHASE

dc.contributor.authorLeroux F.
dc.contributor.authorMoujahid E.M.
dc.contributor.authorRoussel H.
dc.contributor.authorFlank A.-M.
dc.contributor.authorBriots V.
dc.contributor.authorBesse J.-P.
dc.date.accessioned2021-09-28T02:28:14Z
dc.date.available2021-09-28T02:28:14Z
dc.date.issued2002
dc.description.abstractThe substitution in layered double hydroxide-like phases (LDH) of composition (Co2+1-y Cu2+y)2Al3+(OH)6Cl ­· n H2O (0 y 1) was studied by X-ray diffraction and X-ray absorption spectroscopy. It was found that the lamellar character is maintained over the entire range of the substitution. The local order for the composition {Co2Al} is typical of brucite-like sheets, whereas segregation into small domains may explain the results obtained when the percentage of Cu atoms is increased. The {Cu2Al} end-member material presents a local order around the Cu atoms closely related to the botallackite structure as present in basic layered Cu salts, with the presence of two distinct Cu ­Cu distances.
dc.identifierhttps://elibrary.ru/item.asp?id=14041740
dc.identifier.citationClays and Clay Minerals, 2002, 50, 2, 254-264
dc.identifier.issn0009-8604
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/30611
dc.subjectBotallackite Structure
dc.subjectLayered Double Hydroxide
dc.subjectX-ray Absorption Spectroscopy
dc.titleLOCAL ORDER OF THE TRANSITION METALS FOR THE SUBSTITUTION COPPER-ALUMINUM-LAYERED DOUBLE HYDROXIDE-LIKE PHASE
dc.typeСтатья

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