An. Papathanassiou, Investigation of the dielectric relaxation and the transport properties ofporous silicates containing humidity, J PHYS-COND, 12(26), 2000, pp. 5789-5800
The dielectric relaxation responses of pelite, which is a porous silicate s
ediment containing a low content of inherent humidity, were identified and
characterized by employing the experimental scheme of the thermally stimula
ted depolarization current (TSDC) spectroscopy. Comparative experiments wer
e performed on dry samples. The elementary responses that compose the diele
ctric spectrum were recorded by applying certain sampling techniques. The d
ielectric relaxation spectrum consists of two low-temperature mechanisms, w
hich are related to different modes of relaxation of water molecules. A thi
rd one is probably produced by permanent dipoles consisting of point defect
s in the calcium participant. Three relaxation mechanisms were sampled with
in the intermediate temperature region and were strongly affected by the ou
tgassing of the pore network. They correspond to polarization processes occ
urring in the multi-layer shell of humidity over the surface the solid aggr
egates. At higher temperatures, two mechanisms were traced: the first is re
lated to the homogeneous polarization of the specimen as charge carriers mi
grate within conducting territories until they are trapped at internal boun
daries and the latter is described as a long-distance conduction mechanism
which is enhanced by the presence of humidity. The activation energy profil
es of the above-mentioned relaxation mechanisms were obtained from the anal
ysis of the experimental signals of the thermal sampling and the partial he
ating schemes.