The seismic attenuation in concrete has seldom been studied, although it is
an important parameter for survey design. In this paper, the seismic Q fac
tor is estimated from data measured at the Carillon dam. Three methods were
used for this study: amplitude decay yielding a value of 5.1 +/- 1.6, spec
tral ratio giving a value of 8.3 +/- 3.5, and a value of 7.5 +/- 14.9 was o
btained from the rise-time technique. These values are weak compared with w
hat is generally observed in rocks, and slightly lower than values obtained
on laboratory concrete samples. However, the average P wave velocity measu
red on the investigated area is 4081 +/- 95 m.s(-1), an indication of the g
ood quality of the material. Consequently, this strong attenuation could be
attributed on one hand to energy loss, and on the other hand to scattering
caused by the intrinsic cement-aggregate composition of concrete. It is al
so possible that an inadequate sensor coupling had the effect of reducing t
he observed Q value.