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Long-term settlement of the marine foundation due to construction of 1th phase Kansai international airport

机译:关西国际机场一期工程的建立,长期稳定了海洋基础

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A series of elasto-viscoplastic finite element analyses is performed to assess the stress and deformationrnof the marine foundation due to construction of Kansai International Airport (KIA) fill. The foundationrnis modeled by following the stratification at offshore reclamation site. A new concept in terms of occurrencernof viscoplastic behavior even in the quasi-overconsolidated region is incorporated into finite elementrncode in order to simulate the long-term deformation of the Pleistocene clay deposits in Osaka Bay. Attentionrnis also paid to the modeling of permeability for Pleistocene sand gravel layers considering the sedimentationrnenvironment because the performance of excess pore water pressure is strongly dependent on the extent asrnwell as the change in thickness of those permeable sand gravel layers. The mechanism for the propagation ofrnexcess pore water pressure is also discussed. It is very important to know how far the excess pore water pressurerngenerated due to reclamation propagates for assessing the effect of adjacent reclamation on the existingrnreclaimed land. From those findings on the performance of excess pore water pressure, the mode of advancernin settlement of Pleistocene deposits is discussed.
机译:进行了一系列弹黏塑性有限元分析,以评估由于关西国际机场(KIA)填筑而造成的海洋基础的应力和变形。基金会通过在海上填海场进行分层来模拟。为了模拟大阪湾更新世粘土沉积物的长期变形,将一个甚至在准超固结区域的粘塑性行为出现的新概念也纳入了有限元法中。注意,考虑到沉积环境,还需要对更新世砂砾石层的渗透性建模,因为过高的孔隙水压力的表现强烈取决于这些渗透性砂砾石层厚度的变化程度。还讨论了多余孔隙水压力传播的机理。为了评估相邻填海对现有填海土地的影响,了解填海所产生的多余孔隙水的传播程度非常重要。从孔隙水压力过大的研究结果出发,讨论了更新世沉积的超前沉积模式。

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