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Laboratory study of small-strain behavior of a compacted silty sand

机译:密实粉砂的小应变行为的室内研究

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摘要

Small-strain behavior is a key indicator for assessing the performance of compacted fills. Compaction conditions, i.e., initial moisture content and applied energy, govern compaction effectiveness and thus, the structure and matric suction of compacted soil. This paper presents an experimental study of the small-strain behavior of compacted silty sand prepared with different compaction conditions. Specimens with varying initial moisture contents and compaction energies were tested with bender elements to determine the small-strain shear modulus (G0), while the post-compaction matric suction was measured using the filter paper method and tensiometer. The experimental data suggest a pronounced relationship between G0 and the degree of saturation (Sr) of the as-compacted soil specimens. X-ray computed tomography (CT) scans were performed to examine structural changes of selected specimens upon compaction. The laboratory results are also examined in light of common end-product specifications, which show that it is beneficial to compact the soil slightly dry of optimum moisture content from the modulus point of view.
机译:小应变行为是评估压实填料性能的关键指标。压实条件,即初始含水量和施加的能量,决定了压实效果,从而决定了压实土壤的结构和基质吸力。本文介绍了在不同压实条件下制备的压实粉砂的小应变行为的实验研究。使用弯曲元件测试了具有不同初始水分含量和压实能量的样品,以确定小应变剪切模量(G0),同时使用滤纸法和张力计测量了压实后的基质吸力。实验数据表明,G0与压实土壤样品的饱和度(Sr)之间存在明显的关系。进行X射线计算机断层扫描(CT)扫描,以检查压实后所选标本的结构变化。还根据常见的最终产品规格检查了实验室的结果,这些结果表明,从模量的角度来看,压实干燥的土壤要保持最佳水分含量是有益的。

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