首页> 外文期刊>Journal of the Japanese Geotechnical Society >VERIFICATION OF THE ELASTO-VISCOPLASTIC APPROACH ASSESSING THE LONG-TERM DEFORMATION OF THE QUASI-OVERCONSOLIDATED PLEISTOCENE CLAY DEPOSITS
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VERIFICATION OF THE ELASTO-VISCOPLASTIC APPROACH ASSESSING THE LONG-TERM DEFORMATION OF THE QUASI-OVERCONSOLIDATED PLEISTOCENE CLAY DEPOSITS

机译:准超固结更新世粘土沉积物长期变形的弹性-粘弹方法验证

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摘要

A series of elasto-viscoplastic finite element analyses is performed to describe the long-term settlement measured at the reclaimed islands in Osaka Port. The compression modeling for the quasi-overconsolidated Pleistocene clays proposed by the authors has been incorporated to the procedure in which an elasto-viscoplastic deformation is assumed to occur even in the quasi-overconsolidated region (p_0 ≤ p ≤ p_c). One-dimensional analysis is adopted for assessing the settlement of Sakishima and Yumeshima Reclaimed islands, whereas the plane-strain finite element analysis is carried out for investigating the deformation of the Pleistocene deposit beneath the sheet-pile composite revetment at Maishima Reclaimed Island. The proposed procedure is found to provide larger settlement for all cases compared to the conventional approach because of the consideration of viscoplastic deformation in the quasi-overconsolidated region. As for the case of the sheet-pile composite revetment, the effect of stress concentration due to ground improvement with SCP for the Holocene clay layer is remarkable on the underlying Pleistocene deposit. The measured settlement of the individual Pleistocene clay layers as well as the total settlement of the Pleistocene deposits are precisely described by the proposed procedure, whereas the conventional approach in which the instantaneous elastic deformation is assumed to occur in the quasi-overconsolidated region exhibits serious underestimation. From these results, the predictive accuracy of the proposed procedure is verified for assessing the long-term settlement at the reclaimed islands in Osaka Port.
机译:进行了一系列弹黏塑性有限元分析,以描述在大阪港开垦的岛屿上测得的长期沉降。作者提出的准超固结更新世粘土的压缩模型已经被纳入到过程中,在该过程中,即使在准超固结区域(p_0≤p≤p_c)也被假定为发生了弹黏塑性变形。一维分析用于评估Sakishima和Yumeshima再生岛的沉降,而平面应变有限元分析则用于研究Maishima再生岛片状复合护岸下的更新世沉积物的变形。由于考虑了准过度固结区域的粘塑性变形,因此与常规方法相比,所提出的方法可为所有情况提供更大的解决方案。对于片状桩复合护岸的情况,由于全新世粘土层的SCP地面改良而引起的应力集中效应在下层的更新世沉积层上非常明显。通过提出的程序可以精确描述各个更新世粘土层的测量沉降以及更新世沉积物的总沉降,而假定在准超固结区域中发生瞬时弹性变形的传统方法则表现出严重的低估。从这些结果可以验证所提出程序的预测准确性,以评估大阪港开垦岛屿的长期沉降。

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