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Performance of a large-scale slope model subjected to rising and lowering water levels

机译:水位上升和下降的大型边坡模型的性能

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Many slope failures have been observed to occur during times of water level fluctuations. This paper presents a large-scale model test simulating the performance of a sandy silty soil slope subjected to water level rise and drawdown. The slope model is 15 m long, 6 m high and 5 m wide, and the sloping part has an inclination of 1:1 and a height of 4 m. A water level control system was developed to allow the simulation of the rise and sudden drawdown of the water level. Pore-water pressures (negative and positive), total earth pressures, the slip surface and the landslide process were recorded during the simulation process. Data gathered under controlled laboratory conditions was useful for the verification of analytical and numerical modelling methods. Pore-water pressure inside the slope showed a significant delay relative to the drawdown of the water level outside the slope. The failure mode that developed during rapid drawdown was of the multiple retrogressive rotational type. The results provide an improved understanding of the physical behaviour and failure mode of a saturated-unsaturated soil slope subjected to water level fluctuations.
机译:已经观察到在水位波动期间发生了许多边坡破坏。本文提出了一个大型模型试验,模拟了沙质粉质土边坡在水位上升和下降时的性能。边坡模型长15 m,高6 m,宽5 m,倾斜部分的倾角为1:1,高度为4 m。开发了水位控制系统,以模拟水位的上升和突然下降。在模拟过程中记录了孔隙水压力(负压和正压),总土压,滑动面和滑坡过程。在受控实验室条件下收集的数据可用于验证分析和数值建模方法。斜坡内的孔隙水压力相对于斜坡外水位的下降显示出明显的延迟。快速下降期间形成的失效模式是多次回旋旋转类型。结果提供了对饱受水位波动影响的饱和-非饱和土质边坡的物理行为和破坏模式的更好理解。

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