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.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.identifier | https://www.elibrary.ru/item.asp?id=31545717 | |
| dc.identifier.citation | Developments in Clay Science, 2006, 1, C, 309-377 | |
| dc.identifier.doi | 10.1016/S1572-4352(05)01010-X | |
| dc.identifier.issn | 1572-4352 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/44929 | |
| dc.title | CHAPTER 7.3 CLAY MINERAL ORGANIC INTERACTIONS | |
| dc.type | Статья |
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