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dc.contributor.author Carrado K.A.
dc.contributor.author Decarreau A.
dc.contributor.author Petit S.
dc.contributor.author Bergaya F.
dc.contributor.author Lagaly G.
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=31579310
dc.identifier.citation Developments in Clay Science, 2006, 1, C, 115-139
dc.identifier.issn 1572-4352
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44930
dc.description.abstract A subjective differentiation can be made between the formation of clay minerals in their natural, geologic environment such as in soils, and the synthesis of pure minerals in a controlled, laboratory environment. The former point would be of interest to the geochemist, soil scientist, or mineralogist, whereas the latter materials are prepared to exploit a clay mineral’s unique structure and/or surface chemistry for some particular application.
dc.title CHAPTER 4 SYNTHETIC CLAY MINERALS AND PURIFICATION OF NATURAL CLAYS
dc.type Статья
dc.identifier.doi 10.1016/S1572-4352(05)01004-4


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