Novel experimental techniques to measure ultrasonic velocity and atten
uation of surface waves on fluid-filled porous natural rocks are prese
nted. Our experimental results are consistent with the theoretical pre
dictions of Feng and Johnson (1983). Depending on the interface condit
ions, i.e., whether the surface pores are open or closed, pseudo-Rayle
igh, pseudo-Stoneley, and/or true Stoneley surface waves may exist on
fluid-saturated rocks. We have demonstrated the existence of the ''slo
w'' surface wave (true Stoneley mode) on fluid-filled porous rocks wit
h closed surface pores. The velocity and attenuation of the ''slow'' s
urface mode may be used to assess the dynamic permeability of porous f
ormations.