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The uplift behavior of a subway station during different degree of soil liquefaction

机译:不同土壤液化程度的地铁站的隆起行为

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The large underground structures, such as the subway station, deposited in the saturated liquefiable soils are easily subjected to severe damages due to the liquefaction-induced uplift in the strong earthquake. Existing researches of the liquefaction-induced uplift primarily focused on the seismic response of underground structures after soil liquefaction. However, relatively little effort has been dedicated to discussing the uplift behavior in the beginning of soil liquefaction during earthquakes and after soil post-liquefaction when the earthquake stopped. A subway station deposited at different buried depths within different relative density sands suffered from a moderate earthquake was simulated by a Finite Element and Finite Difference (FE-FD) Coupled Method to detect the issue in this study. It was found that soil liquefaction induced by the earthquake loading was a precondition of the uplift trigger, but not a basic reason, both sinking and floatation failure could take place during soil liquefaction. The degree and the area of soil liquefaction surrounding the underground structure and the surrounding soil squeezing into the bottom of the flowing underground structure after seismic liquefaction were the fundamental conditions. The results also showed that when the uplift response occurred, the uplift displacement slowly developed between the elementary liquefaction and the complete liquefaction, and then rapidly developed after the complete liquefaction, but did not cease immediately when the earthquake stopped, whereas still slowly developed, and then settled in some extent with the dissipation of excess pore water pressure.
机译:由于液化引起的强烈地震,沉积在饱和液体土壤中的大地下结构,例如沉积在饱和液体土壤中,沉积在饱和液化土壤中,很容易受到严重的损伤。液化诱导隆起的现有研究主要集中在土壤液化后地下结构的地震反应。然而,相对较少的努力一直致力于讨论地震期间土壤液化开始时的隆起行为以及在地震停止时液化后的土壤液化后。通过有限元和有限差分(FE-FD)耦合方法模拟沉积在不同的相对密度砂内的不同埋藏深度的地铁站,以检测本研究中的问题。结果发现,地震载荷引起的土壤液化是隆起触发的前提,但不是基本原因,在土壤液化过程中可能发生沉没和浮动失败。地下结构围绕地下结构的土壤液化的程度和面积挤压到地震液化后挤压到流动的地下结构底部的底部是根本条件。结果还表明,当发生隆起反应时,升压位移在基本液化和完全液化之间缓慢发展,然后在完全液化后快速发展,但在地震停止时没有停止,而仍然慢慢开发,而且仍然慢慢开发然后在某种程度上在某种程度上溶解过量的孔隙水压。

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