After a reservoir has been in operation for a period of time, a sediment la
yer is likely formed before the dam. Since studies of the effects of sedime
nt layers on the hydrodynamic pressures of impounded water and the aseismic
responses of dam are few, the dynamic effect of sediment may be applied ne
ither in the seismic design of new dams nor in the assessment of earthquake
safety of existing dams. However, a common practice of the action of sedim
ent layers and foundation is based on a partial energy absorption boundary.
It is shown that during a vertical harmonic ground motion, the sediment la
yer could alter the natural frequencies of reservoir. The dynamic pressure
on a rigid vertical dam face caused by the vertical ground motion is obtain
ed through a computational model and an experimental test by using a shakin
g table. With a change in the thickness of sediment, the frequency correspo
nding to the inertia amplification effect appears to vary gradually. The re
sults are useful for further study of seismic responses of dams.