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Geotechnical Hybrid Simulation to Investigate the Effects of the Hydraulic Conductivity on One-Dimensional Consolidation Settlement

机译:岩土力学混合模拟研究水力传导率对一维固结沉降的影响

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摘要

Difficulties in the prediction of time-distribution of consolidation settlement will be introduced by using the Murayama test embankment case of Japan. In particular, it will be discussed why the prediction of consolidation rate is difficult in multi-layered soil with complex and variable mechanical properties like organic soil or peat. It can be inferred that uncertainties, which are embedded intricately in the consolidation problem as well as given ground condition, would be major causes for consolidation settlement. After that, the author focused on the movement of pore water under the various conditions of hydraulic conductivity in the soils, and how it can affect the time-distribution of the consolidation settlement. For the applied key methodology on the consolidation settlement problem, we propose the hybrid consolidation simulation controlling the movement of pore water with high accuracy and, finally, the aim of this article is to discuss the methodological approaches obtained by the study, including the basic concept and accurate movement of pore water under various conditions of soil layers and hydraulic conductivity.
机译:利用日本的村山试验路堤案例将介绍固结沉降时间分布的预测困难。特别地,将讨论为什么在具有复杂且可变的机械特性的多层土壤(如有机土壤或泥炭)中难以预测固结速率。可以推断出,在合并问题中以及给定的基础条件中错综复杂的不确定性将成为合并结算的主要原因。之后,作者重点研究了孔隙水在土壤水力传导率的各种条件下的运动,以及其如何影响固结沉降的时间分布。对于固结沉降问题的应用关键方法,我们提出了一种高精度控制孔隙水运动的混合固结模拟方法,最后,本文的目的是讨论研究获得的方法论方法,包括基本概念。并在各种土壤层和水力传导条件下准确地移动孔隙水。

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