Features of phase formation and phase distribution in the dehydration of coarse gibbsite floccules

dc.contributor.author	Egorova S.
dc.contributor.author	Lamberov A.
dc.date.accessioned	2018-09-18T20:18:47Z
dc.date.available	2018-09-18T20:18:47Z
dc.date.issued	2014
dc.identifier.issn	1070-3632
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/138599
dc.description.abstract	© 2014 Pleiades Publishing, Ltd. A complex study of the phase composition and phase distribution in coarse floccules of the dehydration products of gibbsite thermally treated at atmospheric pressure in air at 250-500°C was performed. The dehydration of gibbsite floccules generates coarsely and finely crystalline boehmite phases. Finely crystalline boehmite is formed by partial "fragmentation" of gibbsite crystals. The layer of coarse boehmite crystals surrounds a finely crystalline boehmite core. χ-Al2O3 predominantly crystallizes on the outer surface of gibbsite particles that contacts with the environment.
dc.relation.ispartofseries	Russian Journal of General Chemistry
dc.subject	alumina
dc.subject	boehmite
dc.subject	dehydration
dc.subject	floccule
dc.subject	gibbsite
dc.title	Features of phase formation and phase distribution in the dehydration of coarse gibbsite floccules
dc.type	Article
dc.relation.ispartofseries-issue	12
dc.relation.ispartofseries-volume	84
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	2364
dc.source.id	SCOPUS10703632-2014-84-12-SID84921710159

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