Field observations in thin soft clay layers may show pore-water pressu
res that increase for some time after the loading is applied. Reasons
for these observations are not well understood. The paper shows how an
elastic viscoplastic constitutive model incorporated into the consoli
dation equation can predict these pore-water pressure increases in soi
ls that exhibit significant creep behaviour (or secondary compression)
. The phenomenon has been related to relaxation in regions of the prof
ile from which drainage has not yet begun.