Recently a new idea for the disintegration of urinary calculi based up
on the large difference of the acoustic impedance inside urinary calcu
li was suggested. This large difference of acoustical impedance betwee
n the two main components of kidney stones, is confirmed in this paper
for smooth laminated uric acid stones by two different experimental t
echniques measuring sound velocities: a surface contact and a submersi
on technique. Our measured values correlate well with the large differ
ences of the earlier reported measured sound velocities. In general, t
he disintegration of a urinary stone can be described as follows: a ur
inary calculus is an inhomogeneous geometrical structure, and its stru
cture plays an important role in the disintegration process.