CHAPTER 7.2 THERMALLY MODIFIED CLAY MINERALS

dc.contributor.author	Heller-Kallai L.
dc.date.accessioned	2024-09-22T02:54:10Z
dc.date.available	2024-09-22T02:54:10Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=17810268
dc.identifier.citation	Developments in Clay Science, 2006, 1, C, 289-308
dc.identifier.issn	1572-4352
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/45318
dc.description.abstract	The structure and composition of clay minerals are modified by heating. The concomitant changes in properties can be exploited for practical purposes. The actual temperatures at which changes occur vary greatly from one clay mineral group to another, and even for different specimens within a given group. These temperatures also depend on the particle size and on the heating regime. Four principal temperature ranges in which significant changes occur in the structures of clay minerals may be distinguished.
dc.title	CHAPTER 7.2 THERMALLY MODIFIED CLAY MINERALS
dc.type	Статья
dc.identifier.doi	10.1016/S1572-4352(05)01009-3

Files in this item

Name: Hell_06.pdf

Size: 301.8Kb

Format: PDF