CHAPTER 7.3 CLAY MINERAL ORGANIC INTERACTIONS

dc.contributor.author	Lagaly G.
dc.contributor.author	Ogawa M.
dc.contributor.author	Dékány I.
dc.date.accessioned	2024-09-04T09:55:40Z
dc.date.available	2024-09-04T09:55:40Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=31545717
dc.identifier.citation	Developments in Clay Science, 2006, 1, C, 309-377
dc.identifier.issn	1572-4352
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/44929
dc.description.abstract	Clay minerals can react with different types of organic compounds in particular ways. Kaolin species (kaolinite, nacrite, and dickite) adsorb particular types of neutral organic compounds between the layers. The penetration of organic molecules into the interlayer space of clay minerals is called intercalation. Intercalated guest molecules can be displaced by other suitable molecules.
dc.title	CHAPTER 7.3 CLAY MINERAL ORGANIC INTERACTIONS
dc.type	Статья
dc.identifier.doi	10.1016/S1572-4352(05)01010-X

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