带粘性回填土的柔性悬臂式挡土墙地震行为数值研究

Bouraida El Yamouni, Fadoua El Khannoussi, A. Khamlichi
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摘要

在对保留粘性回填土的柔性悬臂墙进行抗震设计时,通常的做法是忽略粘性效应。动侧向土压力通常是根据主要针对无粘性土的方法或通过假静力分析方法进行评估的。然而,实验和理论证据都表明,这些方法都没有考虑到土壤内聚力的显著影响。本研究对高度为 5.4 米的柔性悬臂墙进行了有限元建模(FE),该墙在初始静荷载和地震荷载作用下支撑着均质粘性回填土。然后将计算出的主动土推力与通过实验和传统分析方法获得的数值进行比较。结果表明,土壤内聚力的存在大大降低了地震对柔性悬臂挡土墙的要求,使地震作用土压力和总地震推力分别大幅降低了 50%和 52%。它还通过将地震推力的作用点向墙基移动,提高了系统的整体稳定性,从而增加了安全系数。此外,它还大大减少了墙体在墙干顶部的位移,与无粘性回填土相比,位移减少高达 104%。据观察,一些抗震法规推荐的传统方法在很大程度上低估了地震活动压力。
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Numerical Investigation of Seismic Behaviour for a Flexible Cantilever Retaining Wall with Cohesive Backfill
In the seismic design of flexible cantilever walls retaining cohesive backfill soil, the common practice is to neglect the cohesion effect. Dynamic lateral earth pressure is typically evaluated based on approaches primarily intended for cohesionless soils or through analytical pseudo-static methods. Nevertheless, both experimental and theoretical evidence has demonstrated significant effects due to soil cohesion that are not accounted for by these methods. This study involved finite element modeling (FE) of a flexible cantilever wall with a height of 5.4m, supporting homogeneous cohesive backfill under initial static and seismic loadings. The calculated active earth thrust was then compared with values obtained experimentally and through conventional analytical methods. The obtained results indicate that the presence of soil cohesion significantly reduces seismic demands on flexible cantilever retaining walls, resulting in a substantial reduction of seismic active earth pressures and total seismic thrust by up to 50% and 52%, respectively. It enhances also the overall stability of the system by shifting the point of application of seismic thrust toward the base of the wall, thereby increasing the safety margin. In addition, it significantly decreases the wall displacement at the stem top, with reductions of up to 104% compared with the case involving cohesionless backfill. It was observed that the conventional methods recommended by some seismic regulations largely underestimate seismic active pressure.
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