포화된 정규압밀 점성토에서 비배수 공극수압의 거동(Ⅱ) - 점탄성 해석 모델 -

Abstract

The initial condition of is used for analyzing the time dependent behavior of ground. This is based on the concept that the coefficient of pore water B is the unity on the condition of saturation. but some measured consolidation data in the field showed that the pore water pressure was not dissipated as time elapsed but it was maintained constant value or it's dissipation rate was slower than that of the predicted. and so the measured data of pore water pressure was not consistent with that of settlement. In this study, the rheological model for the pore water pressure behavior on undrained condition was induced and compared with the experiment data of the literature. The result showed that the suggested model was consistent well with the result of experiment. but the suggested model could not explain the effect of the decrease of void ratio according to consolidation.