The attenuation of an ultrasonic wave in porous rocks has been measure
d by means of a spectral analysis technique in the frequency range 100
kHz-1 MHz. Experimental results, after compensation for the geometric
divergence of the emitted ray beam, are presented for three types of
rocks. They display two characteristics, essentially related to the na
ture and the structure of the probes: the quality factor Q does not de
pend on frequency (Q is Fairly constant in the whole range of explorat
ion); and the attenuation remains high. Experimental data are also com
pared to predictions obtained from different models, but only Stoll's
composite model gives predictions in fair agreement with experiments.