Seismically Induced Delayed-Landslides in Homogeneous Cohesive Slopes and Embankments

Project is designed to track the pore pressure generation/dissipation as a function of varying shaking events. These pore pressure regimes are studied for their long term (multiple hours/days) contribution to instability in homogeneous normally consolidated clay slopes.

本项目旨在追踪孔隙水压力（pore pressure）的产生与消散过程随不同振动事件变化的规律。针对此类孔隙水压力状态，本研究探究其在长期（数小时至数天）尺度下对均质正常固结黏土边坡失稳的影响机制。