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Ground Improvement Reinforcement Mechanisms Determined for the Mw7.8 Muisne, Ecuador, Earthquake

机译:确定厄瓜多尔Muisne Mw7.8地震的地面加固加固机制

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The 2016 Muisne, Ecuador, earthquake caused widespread soil liquefaction and structural damage as affected sites were subject to peak ground accelerations of greater than 0.4 g. Liquefaction was observed in the silty sand foundation soils adjacent to the recently constructed Briceno Bridge embankment site as evidenced by sand boils and liquefaction ejecta. However, the nearly 1 km long Briceno embankment, whose foundation materials were reinforced by relatively widely spaced rammed aggregate pier ground improvement elements, exhibited only minor damage after shaking. Post-earthquake data indicated that the ground improvement works provided densification of the SM foundation soils. This densification was not sufficient, however, to fully explain the stability of the embankment, an achievement that necessitates the presence of other stabilization mechanisms. This paper is of particular significance because it presents proposed stabilization methods that reach beyond densification in difficult to densify soils such as silty sands and sandy silts.
机译:2016年厄瓜多尔Muisne地震造成广泛的土壤液化和结构破坏,因为受灾地点的地面加速度峰值超过0.4 g。在靠近新近建造的Briceno桥路堤现场的粉质砂土土壤中观察到了液化现象,沙沸腾和液化喷出物证明了这一点。但是,将近1公里长的Briceno路堤,其地基材料由相对较宽的夯实的集料墩墩台地面改良材料加固,震荡后仅表现出较小的损坏。地震后的数据表明,地面改良工作为SM基础土壤提供了致密化作用。然而,这种致密化不足以充分说明路堤的稳定性,这一成就需要其他稳定机制的存在。本文具有特别的意义,因为它提出了拟议的稳定化方法,该方法在难以致密的土壤(如粉砂和沙质粉土)中已超越了致密化。

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