dc.contributor.author |
Lounev I. |
|
dc.contributor.author |
Nigmatullin R. |
|
dc.contributor.author |
Zavidonov A. |
|
dc.contributor.author |
Gusev Y. |
|
dc.contributor.author |
Manurov I. |
|
dc.contributor.author |
Kaumov S. |
|
dc.contributor.author |
Muslimov R. |
|
dc.date.accessioned |
2018-09-17T20:23:33Z |
|
dc.date.available |
2018-09-17T20:23:33Z |
|
dc.date.issued |
2002 |
|
dc.identifier.issn |
0022-3093 |
|
dc.identifier.uri |
https://dspace.kpfu.ru/xmlui/handle/net/133442 |
|
dc.description.abstract |
The measurements of the imaginary part of the complex susceptibility in water-saturated sands and clays have been conducted. To explain the experimental data obtained the fractal model of medium has been used [Laboratory Humidity Ovens (Non-injection Type), BS (1964) 3718; Fleches du temps et geometric fractale, Paris Hermes, 1998]. In the range of humidity not exceeding 12%, the main contribution to the dipole relaxation is provided has bound water [A Wetting Ability Clays and Clay Minerals, Kiev, 1961, p. 292], that is reflected in the power-law exponent behavior. © 2002 Elsevier Science B.V. All rights reserved. |
|
dc.relation.ispartofseries |
Journal of Non-Crystalline Solids |
|
dc.title |
Analysis of dielectric relaxation data in water-saturated sands and clays |
|
dc.type |
Conference Paper |
|
dc.relation.ispartofseries-issue |
1-3 |
|
dc.relation.ispartofseries-volume |
305 |
|
dc.collection |
Публикации сотрудников КФУ |
|
dc.relation.startpage |
255 |
|
dc.source.id |
SCOPUS00223093-2002-305-13-SID0036642612 |
|