地震荷载下淤泥质砂中基于能量的孔隙压力生成模型

G. Tomasello, D. Porcino
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摘要

地震期间,饱和淤泥质砂中产生的过剩孔隙水压力会导致土壤的抗剪强度降低,甚至液化。为了探索影响非塑性淤泥质砂基于能量的过剩孔隙水压力产生模型的关键因素,我们开展了一项综合实验计划,包括不排水循环单剪试验。所研究的影响因素包括非塑性细粒含量(小于和大于临界值≅25%)、堆积密度、垂直有效应力、外加循环应力比和土壤结构。研究发现,过剩孔隙水压力比与单位体积耗散能量之间的关系主要取决于土壤的相对密度和细粒含量,而循环应力比、初始垂直有效应力和土壤结构(即重组方法)似乎影响较小。建议对 Berrill 和 Davis 针对洁净砂土开发的基于能量的原始模型进行修订,以提高残余过剩孔隙水压力与归一化累积耗散能量的预测精度。对修订模型的校准参数进行了非线性多变量回归分析,以建立相关关系。最后,通过在 2012 年意大利艾米利亚-罗马涅地震后发生液化的一个地点对不同的淤泥质砂进行额外的循环简单剪切试验,对这些相关性进行了验证。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Energy-Based Pore Pressure Generation Models in Silty Sands under Earthquake Loading
During an earthquake, excess pore water pressure generation in saturated silty sands causes a reduction in shear strength and even liquefaction of the soil. A comprehensive experimental program consisting of undrained cyclic simple-shear tests was undertaken to explore the key factors affecting the energy-based excess pore water pressure generation models for non-plastic silty sands. The examined influencing factors were non-plastic fines content (less than and greater than the threshold value ≅ 25%), packing density, vertical effective stress, applied cyclic stress ratio, and soil fabric. The relationship between excess pore water pressure ratio and dissipated energy per unit volume was found to be mainly dependent on the relative density and fines content of soil, whereas the cyclic stress ratio, initial vertical effective stress, and soil fabric (i.e. the reconstitution method) appeared to have a minor impact. A revision of the original energy-based model developed for clean sand by Berrill and Davis was proposed to improve prediction accuracy in terms of residual excess pore water pressures versus normalised cumulative dissipated energy. Nonlinear multivariable regression analyses were performed to develop correlations for the calibration parameters of the revised model. Lastly, these correlations were validated through additional cyclic simple-shear tests performed on different silty sands recovered at a site where liquefaction occurred after the 2012 Emilia Romagna (Italy) earthquake.
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