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Measurement of Small-Strain Shear Moduli of Partially Saturated Sand During Infiltration in a Geotechnical Centrifuge

机译:岩土离心机入渗过程中部分饱和砂土的小应变剪切模量的测量

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This paper describes the use of bender elements to measure changes in small strain shear modulus, G_max, of sand layers due to the change in degree of saturation during centrifuge tests. The goal of the measurements is to verify that steady-state infiltration is an appropriate technique to control the effective stress in centrifuge physical modeling of partially saturated sands. Specifically, the suitability of infiltration is assessed by checking if the measured values of G_max of partially saturated sand layers follow a similar trend to dry and saturated sand layers when the effective stress is defined from the suction and degree of saturation profiles during steady-state infiltration. Three pairs of bender elements were installed at different depths in a container of Ottawa sand, and the shear wave velocities of the sand were measured during steady-state infiltration into the sand layer. The applied infiltration rate was varied to obtain different uniform distributions of degrees of saturation with depth. Consistent with results from suction-controlled resonant column tests performed on the same sand, the values of G_max measured from the bender element tests varied nonlinearly with degree of saturation with a peak value at a degree of saturation between 0.3 and 0.4. When interpreted in terms of mean effective stress, the values of G_max from the bender element tests on partially saturated sands followed a unique trend consistent with measurements for dry and saturated sands.
机译:本文介绍了使用弯曲元件来测量由于离心测试过程中饱和度变化而引起的砂层小应变剪切模量G_max的变化。测量的目的是验证稳态渗透是控制部分饱和砂离心机物理模型中有效应力的一种合适技术。具体而言,当从稳态渗透过程中的吸力和饱和度曲线定义有效应力时,通过检查部分饱和砂层的G_max的测量值是否遵循与干燥和饱和砂层相似的趋势,可以评估渗透的适用性。将三对弯曲器元件安装在渥太华沙子容器中的不同深度处,并在稳态渗入砂层的过程中测量了沙子的剪切波速度。改变所施加的渗透速率以获得饱和度随深度的不同均匀分布。与在同一砂子上进行的吸力控制共振柱测试的结果一致,从弯曲元件测试测得的G_max值随饱和度呈非线性变化,峰值在0.3至0.4之间。当用平均有效应力来解释时,来自对部分饱和的砂岩进行弯曲元素测试的G_max值遵循与干燥和饱和砂岩测量一致的独特趋势。

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