The generation of ultrasound in a porous water-saturated medium subjected t
o rapid electromagnetic heating is considered. The irradiation provides the
Joule heating of narrow and electrically high resistive pore throats, whic
h interconnect cavities within the medium and, consequently, determine the
permeability of the medium. Because of the small throat sizes, the sound ge
neration is accompanied by considerable thermal flows going out from the th
roats into a relatively cold environment. Due to the latter, the output of
the ultrasonic measurement allows one to estimate the rate of the thermal e
xchange process. A common geometric model of fluid flows and electric curre
nts throughout a complicated network of intergranular cavities and their in
terconnecting throats is used for calculating the permeability of a rock on
the basis of the determined values of the thermal exchange rate. (C) 2001
MAIK "Nauka/Interperiodica".