DEHYDRATION BEHAVIORS OF INTERLAYER WATER IN SYNTHETIC BUSERITES

dc.contributor.authorChoi H.S.
dc.contributor.authorKim S.J.
dc.contributor.authorKim J.J.
dc.date.accessioned2022-10-20T08:59:37Z
dc.date.available2022-10-20T08:59:37Z
dc.date.issued2004
dc.description.abstractThe structural changes of synthetic buserites (10Å phases), hydrous phyllomanganates, have been studied as a function of exchangeable interlayer cations and the relative humidity (RH) at which the sample is equilibrated. This study shows that the basal spacing of buserites and their-dehydration products vary depending on the nature of interlayer cations and water molecules. Na-buserite transforms directly to 7Å phase even in air dry. Cabuserite does not easily transform to 7Å phase even in a low RH. With increasing temperature, Mg-buserite transforms very slowly through progressive intermediate phases to 7Å phase at about 200°C, whereas Zn-buserite transforms directly to 7Å phase at about 60°C. Both Mg-and Zn-buserites do not dehydrate to 7Å phase even in a very low RH.
dc.identifierhttps://elibrary.ru/item.asp?id=14413580
dc.identifier.citationGeosciences Journal, 2004, 8, 3, 273-279
dc.identifier.issn1226-4806
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38978
dc.titleDEHYDRATION BEHAVIORS OF INTERLAYER WATER IN SYNTHETIC BUSERITES
dc.typeСтатья

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