Relation between electric properties and water saturation for hematitic sandstone with frequency

This paper focuses on the effect of water saturation on A. C. electrical conductivity and dielectric constant of
 fully and partially saturated hematitic sandstone sample (Aswan area, Egypt). The saturation of the sample was
 changed from partial to full saturation. Complex resistivi...

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Bibliographic Details
Main Author: M. M. Gomaa
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2008-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3015
Description
Summary:This paper focuses on the effect of water saturation on A. C. electrical conductivity and dielectric constant of
 fully and partially saturated hematitic sandstone sample (Aswan area, Egypt). The saturation of the sample was
 changed from partial to full saturation. Complex resistivity measurements at room temperature (~16°C), were
 performed in the frequency range from 0.1 Hz to 100 KHz. Experimental electrical spectra indicate, generally,
 that the electrical conductivity and dielectric constant vary strongly with water saturations and frequency. The
 low frequency electrical conductivity and dielectric constant are mainly controlled by surface conduction and
 polarization of the electrical double layer. The behaviour of the electrical conductivity and dielectric constant,
 with increasing water content, were argued to the orientational polarization of bound water for very low saturations,
 displacement of the excess surface charges for relatively low saturations, and free exchange of excess ions
 in double layer with the bulk electrolyte and generation of transient diffusion potentials which lag behind the
 applied field for high saturations.
ISSN:1593-5213
2037-416X