The effect of pore fluid viscosity on the stiffness, damping, and liquefact
ion characteristics of sands was investigated to assess the potential contr
ibutions to a centrifuge model seismic response for soils saturated with hi
gh-viscosity pore fluid. Resonant column tests with cyclic loading frequenc
ies in the range of 20-45 Hz were performed on a variety of fluids and sand
sizes. At a strain level less than 7, x 10(-4), the damping increased with
pore fluid viscosity and shear strain amplitude, and it decreased with san
d particle size. However, at shear strain greater than about 2 X 10(-4), th
e increased skeleton damping tended to mask any effect of additional dampin
g due to fluid viscosity. The liquefaction tests on fine silica sand reveal
ed that the increase in total energy dissipation was not more than 10% for
100 cS oil when compared with water at a driving frequency of 25 Hz. Based
on the experimental results, a simple model is proposed to examine the depe
ndency of viscous damping on pore fluid viscosity, loading frequency, parti
cle size, and shear strain amplitude.