The dielectric properties of low porosity polycrystalline marble and granit
e rocks were investigated using broadband dielectric relaxation spectroscop
y (10(-2)-10(6) Hz) at fixed room temperature (295 K). The water content of
the specimens was varied between 0 and 0.22 % (mass of absorbed water per
mass of dry rock material %). The dielectric relaxation spectra were found
to exhibit large low-frequency dispersion that depends strongly on the wate
r content. A thorough study of this dispersion reveals that the main part o
f the enhanced epsilon* values originates from bulk effects.