The effect of clay morphology on water relaxation

dc.contributor.author	Lunev I.
dc.contributor.author	Nigmatullin R.
dc.contributor.author	Zavidonov A.
dc.contributor.author	Gusev Y.
dc.contributor.author	Manyurov I.
dc.date.accessioned	2018-09-17T21:14:32Z
dc.date.available	2018-09-17T21:14:32Z
dc.date.issued	2001
dc.identifier.issn	1063-7842
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/134720
dc.description.abstract	The frequency dependence of the permittivity of water in calcium kaolinite (clay) is measured. It is shown that two mechanisms contribute to dipole relaxation of water. One refers to water in the free volume of pores in the clay. The other is associated with bound water covering the porous surface. Experimental data are treated in terms of a fractal model of the medium. The frequency dependence of the permittivity in a wide range of water content in the clay is accounted for theoretically. © 2001 MAIK "Nauka/Interperiodica".
dc.relation.ispartofseries	Technical Physics
dc.title	The effect of clay morphology on water relaxation
dc.type	Article
dc.relation.ispartofseries-issue	11
dc.relation.ispartofseries-volume	46
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	1473
dc.source.id	SCOPUS10637842-2001-46-11-SID0035541612

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.