The dielectric relaxation responses of pelite, which is a porous silicate
sediment containing a low content of inherent humidity, were identified and
characterized by employing the experimental scheme of the thermally stimulated
depolarization current (TSDC) spectroscopy. Comparative experiments were
performed on dry samples. The elementary responses that compose the dielectric
spectrum were recorded by applying certain sampling techniques. The dielectric
relaxation spectrum consists of two low-temperature mechanisms, which are
related to different modes of relaxation of water molecules. A third one is
probably produced by permanent dipoles consisting of point defects in the calcium
participant. Three relaxation mechanisms were sampled within the intermediate
temperature region and were strongly affected by the outgassing of the pore
network. They correspond to polarization processes occurring in the multi-layer
shell of humidity over the surface the solid aggregates. At higher temperatures,
two mechanisms were traced: the first is related to the homogeneous polarization
of the specimen as charge carriers migrate within conducting territories until
they are trapped at internal boundaries and the latter is described as a
long-distance conduction mechanism which is enhanced by the presence of
humidity. The activation energy profiles of the above-mentioned relaxation
mechanisms were obtained from the analysis of the experimental signals of the
thermal sampling and the partial heating schemes.