首页> 外文期刊>Soils and foundations >NUMERICAL ASSESSMENT FOR THE BEHAVIOR OF THE PLEISTOCENE MARINE FOUNDATIONS DUE TO CONSTRUCTION OF THE 1ST PHASE ISLAND OF KANSAI INTERNATIONAL AIRPORT
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NUMERICAL ASSESSMENT FOR THE BEHAVIOR OF THE PLEISTOCENE MARINE FOUNDATIONS DUE TO CONSTRUCTION OF THE 1ST PHASE ISLAND OF KANSAI INTERNATIONAL AIRPORT

机译:关西国际机场一期岛建设中的更新世海洋基金会行为的数值评估

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摘要

A series of elasto-viscoplastic finite element analyses is performed to assess the stress and deformation of the Pleistocene marine foundation due to construction of the 1st phase island of Kansai International Airport in Osaka Bay. Attention is paid to the modeling of permeability for Pleistocene sand gravel layers considering the sedimentation environment because the performance of excess pore water pressure is strongly dependent on the extent of distribution as well as the change of thickness of those permeable sand gravel layers. The concept of "mass permeability" is introduced to model the actual process of dissipation of excess pore water pressure in the field. The mechanism for the propagation of excess pore water pressure is also discussed. Special attention is given to the modeling of the compressibility of the highly structured Pleistocene clay layers, exhibiting already significant visco-plastic deformations even in the quasi-overconsolidated effective stress range. The present numerical analyses are found to describe the large and long-term settlement together with the slow dissipation of excess pore water pressure in the Pleistocene clay and sand gravel layers that actually has taken place in the field. A detailed comparison of the distribution of excess pore water pressure and the differential compression for the individual Pleistocene clay layers shows that the calculated performance can well describe the actual behavior of the Pleistocene deposits due to the construction of the 1st phase island of Kansai International Airport.
机译:进行了一系列弹黏塑性有限元分析,以评估由于大阪湾关西国际机场第一阶段岛的建造而导致的更新世海洋基础的应力和变形。考虑到沉积环境,要注意更新世砂砾石层渗透性的建模,因为过高的孔隙水压力的性能强烈取决于这些渗透性砂砾石层的分布程度以及厚度的变化。引入“质量渗透率”的概念来模拟现场多余孔隙水压力消散的实际过程。还讨论了过量孔隙水压力传播的机理。特别注意高度结构化的更新世粘土层的可压缩性建模,即使在准过度固结的有效应力范围内,也已经表现出显着的粘塑性变形。发现目前的数值分析可以描述大块和长期沉降,以及在该油田实际发生的更新世粘土层和砂砾层中超孔隙水压力的缓慢消散。对各个更新世粘土层的多余孔隙水压力分布和压差的详细比较表明,由于关西国际机场第一阶段岛的建设,所计算的性能可以很好地描述更新世沉积物的实际行为。

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