Screening-level studies indicated large zones of the foundation soil b
eneath Duncan Dam could be triggered to liquefy under the design earth
quake, resulting in flow slides that could lead to breaching of the da
m. In these studies, estimates of the key soil parameters were obtaine
d from an indirect procedure using penetration tests and Seed's chart,
which is based on field experience during past earthquakes together w
ith empirical correction factors for high confining stress and static
bias. This is state-of-the-practice procedure in North America and is
used because of the difficulty in retrieving and testing undisturbed s
amples of sand. With the high confining stresses present at the site,
the indirect approach gave very low values of the key liquefaction pro
perties of the soil, and the use of such low values in analyses indica
ted that major and costly remedial measures were required. Thus a more
direct approach was undertaken. This involved both direct and semidir
ect determination of the key soil parameters through an extensive labo
ratory study based on testing of undisturbed samples obtained by freez
ing in situ. The results showed that both the triggering resistance an
d the residual strength values of the soil were very much higher than
those obtained from the indirect approach. Analyses carried out using
direct measurement of the key soil parameters indicated that the dam,
in fact, would be stable.