An important factor in evaluating the stability of hydraulic fills aga
inst flow sliding is the undrained steady-state strength mobilized in
the field. This paper proposes an empirical relationship between three
factors: the undrained strength back-calculated from fills that faile
d by flow sliding, equivalent clean sand normalized blow-count values,
and soil-specific parameters from steady-state laboratory testing. It
is shown that S-uo, which is a reference value of steady-state streng
th at maximum void ratio, is an important soil parameter. The proposed
method offers an explanation for the performance of many artificial s
and islands in the Beaufort Sea, indicates the extreme sensitivity of
S-uo to soil type and the usefulness of S-uo for assessing the potenti
al strength loss of soils for use in safety assessments of existing hy
draulic fills.