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The effect of clay morphology on water relaxation

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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.

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