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Post-liquefaction settlement analyses based on the volume change characteristics of undisturbed and reconstituted samples

机译:基于未扰动和重构样本的体积变化特征的液化后沉降分析

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摘要

Available data on post-liquefaction volumetric strain were collected from the results of tests conducted in several laboratories on both undisturbed samples and reconstituted samples. The volume change characteristics were found to depend significantly on the degree of disturbance during the undrained cyclic loading preceding the drainage. Its effect was shown to be expressed quantitatively by way of the maximum shear strain, gamma(max), as an index parameter. Charts were prepared for the volumetric strain as a function of the ranges in relative density and void ratio considering two levels of disturbance, as expressed by gamma(max) =4.13% and 10%. These charts were provided for each post liquefaction volumetric strain in association with the reconstituted and undisturbed samples. By postulating the former to represent the performance of recent man-made fills and the latter to represent that of alluvial or diluvial deposits, simple analyses were conducted to estimate the settlements of the ground surface at five sites which were affected by liquefaction during the 2011 East Japan Earthquake. A comparison of these estimated values with those actually observed indicated a reasonable level of agreement. Four sites where compaction piles had been installed were also chosen for similar analyses. Both the observed and the estimated settlements were small, namely, in the order of a few centimetres, which also indicates mutual coincidence as a whole. (C) 2016 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V. All rights reserved.
机译:液化后体积应变的可用数据是从几个实验室对未搅动样品和重构样品进行的测试结果中收集的。发现体积变化特征很大程度上取决于排水之前不排水的循环荷载作用下的扰动程度。它的作用已显示为通过最大剪切应变gamma(max)作为指标参数来定量表示。考虑到两个干扰水平,以γ(max)= 4.13%和10%表示的形式,针对体积应变绘制了相对密度和空隙率范围的函数的图表。这些图表是为每个液化后体积应变以及重构和未扰动的样品提供的。通过假定前者代表最近的人造填充物的性能,并假设后者代表冲积或冲积沉积物的性能,进行了简单的分析,以估算在2011年东部受液化影响的五个地点的地表沉降日本地震。将这些估计值与实际观察到的值进行比较,可以得出合理的协议水平。还选择了四个安装压实桩的地点进行类似分析。观测到的和估计的沉降都很小,即大约几厘米,这总体上也表明了彼此的巧合。 (C)2016年日本岩土学会。 Elsevier B.V制作和托管。保留所有权利。

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