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Experimental study of laterite soil slope influenced by water level fluctuation

机译:水位波动对红土边坡影响的试验研究

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Failure of slopes is often caused by seasonal water level fluctuation of reservoirs. To examine the impacts of water level fluctuation in water rising and drawdown stage, a slope model test is presented using the laterite soil. The controlling of rising and drawdown of water level is implemented in the test, and a series of test data such as pore water pressure, water content and displacement are obtained during the simulation process. The results indicate that the pore water pressure responses delay with the rising and drawdown water level. The water content gradually increases from the trailing edge. The mechanism of deformation and instability are revealed by the experiment under water level fluctuation. The results indicate that the displacement in the vertical direction is much larger than that in the horizontal direction under the condition of water level fluctuation, especially in water rising stage. The water rise and drawdown gradually softening will lead to the strength reduction and therein induce larger deformation.
机译:斜坡的破坏通常是由水库季节性水位波动引起的。为了检查水位波动对水上升和下降阶段的影响,使用红土土壤进行了边坡模型测试。试验实现了水位上升和下降的控制,在模拟过程中获得了孔隙水压力,含水量和排水量等一系列试验数据。结果表明,孔隙水压力响应随水位的上升和下降而延迟。含水量从后缘逐渐增加。在水位波动下,实验揭示了变形和失稳的机理。结果表明,在水位波动的条件下,特别是在涨水阶段,垂直方向的位移远大于水平方向的位移。上升和下降的水逐渐软化将导致强度降低,并在其中引起较大的变形。

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