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Soil Particle Movement and Shear Band Development during Plane Strain Compression

机译:平面应变压缩过程中的土壤颗粒运动和剪切带发展

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Most geotechnical structures failed by formation and development of shear bands in soils. Thus, shear deformation and shear bands development evaluation are necessary to understand shear failure mechanism. During shearing, deformation behaviour analysis for soil particles within entire soil specimen are evaluated to understand the soil behaviour and shear strength characteristics. In this paper, a series of plane strain compression tests using Nevada sand and Ottawa sand were conducted to identify the shear strain and shear failure mechanism. With the results of plane strain compression tests, image analyses using Particle Image Velocimetry (PIV) were carried out in order to measure the change in position of soil particles and shear bands development. Deformation vectors and contours were constructed to see the entire deformation mechanism in the soil specimen. During shearing, shear band was identified after peak stress and most visually distinctive at residual state. However, shear band started to develop invisibly immediately after starting loading and this invisible development was able to be observed by horizontal and vertical movement analyses of PIV. Soil particles moved actively in horizontal and vertical direction to generate shear band in the beginning of shearing. After development of shear band, soil particles moved along the shear band.
机译:大多数岩土结构由于在土壤中形成剪切带而失效。因此,剪切变形和剪切带发展评价是了解剪切破坏机理的必要条件。在剪切过程中,对整个土壤样本中土壤颗粒的变形行为分析进行了评估,以了解土壤行为和抗剪强度特性。本文通过内华达砂和渥太华砂进行了一系列平面应变压缩试验,以确定剪切应变和剪切破坏机理。根据平面应变压缩测试的结果,使用粒子图像测速仪(PIV)进行了图像分析,以测量土壤颗粒位置的变化和剪切带的发展。构造了变形矢量和轮廓,以查看土壤样本中的整个变形机理。在剪切过程中,剪切带在峰值应力之后被识别,并且在残余状态下在视觉上最具特色。但是,剪切带在开始加载后立即开始无形地发展,这种不可见的发展可以通过PIV的水平和垂直运动分析来观察。土壤颗粒在水平和垂直方向上主动运动,在剪切开始时产生剪切带。剪切带形成后,土壤颗粒沿着剪切带移动。

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