Abstract
The results of the measurement of relative complex dielectric permittivity over a wide frequency range (from 20 Hz to 20 GHz) solid sandy rocks and two samples of destroyed sandy rocks, saturated with distilled water, are presented. It is shown that at frequencies above 100 MHz, the samples have differences in the values of the real part of the RCP and specific electrical conductivity due to differences in specific surface area and porosity.
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