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A semi-empirical model to predict excess pore pressure generation in partially saturated sand

机译:一种半经验模型,以预测部分饱和沙子的过度孔隙压力产生

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Past studies revealed that excess pore pressure generation due to cyclic loading is highly governed by induced strains, volumetric deformation potential of soil, number of cycles, and bulk stiffness of pore fluid. It is well established that partial saturation can significantly reduce bulk stiffness of pore fluid and consequently excess pore pressure generation during seismic loading. On the basis of that, a number of researchers have investigated induced partial saturation as an effective soil improvement technique to increase the liquefaction resistance of fully saturated soils. This paper focuses on development of a semi- empirical model to interpret the effects of partial saturation on the excess pore pressure generation in sands. In this regard, an existing strain based excess pore pressure ratio (r_(u)) prediction model originally developed for fully saturated soils was modified to incorporate the effect of partial saturation on the excess pore pressure generation. The literature data as well as data from a series of strain-controlled direct simple shear test were used to evaluate the reliability of the proposed equation in predicting the excess pore pressure ratio in partial saturation condition.
机译:过去的研究表明,由于循环载荷引起的过量的孔隙压力由诱导菌株,土壤的体积变形电位,循环数量和孔隙流体的大量刚度的高度治理。很好地确定,部分饱和可以显着降低孔隙流体的体积刚度,从而在地震载荷期间过量的孔隙压力产生。在此基础上,许多研究人员已经研究了诱导的部分饱和度作为一种有效的土壤改善技术,以增加完全饱和土壤的液化抗性。本文侧重于开发半经验模型,以解释部分饱和对砂岩中过量孔隙压力产生的影响。在这方面,修饰了最初为完全饱和土壤开发的基于菌株的过量孔隙压力比(R_(U))预测模型掺入了部分饱和对多余孔隙压力产生的影响。文献数据以及来自一系列应变控制的直接简单剪切试验的数据用于评估所提出的方程在部分饱和条件下预测过量孔隙压力比的可靠性。

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