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On the determination and evolution of fabric in representative elementary volumes for a sand specimen in triaxial compression

机译:三轴压缩砂试样代表性基本体积织物的测定和演化

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Abstract The soil response in triaxial compression tests, that are commonly treated as element tests, is known to be inhomogeneous. Several studies have revealed the localisation of deformation throughout the whole specimen by digital image correlation techniques on X-ray tomographies. The fabric of a soil specimen has so far only been studied on complete specimens as a bulk measurement or in chosen subsets. In this contribution, we present a study on the spatial and temporal distribution of the fabric throughout one Hostun sand sample in triaxial compression. Therefore, we calibrated the minimum representative element size first for three chosen fabric variables considering three different criteria. By distributing the elements in a regular grid over the specimen, we are able to clearly identify the onset of the localisation in terms of void ratio, coordination number and contact fabric anisotropy. Spatially and temporally the contact fabric variables precede the void ratio changes as they are much more sensitive to small changes.Graphical Abstract
机译:摘要 三轴压缩试验中的土体响应通常被视为单元试验,是不均匀的。几项研究揭示了通过X射线断层扫描上的数字图像相关技术在整个标本中变形的局部化。到目前为止,土壤试样的结构仅作为整体测量或选定的子集在完整试样上进行研究。在这篇文章中,我们提出了一项关于织物在三轴压缩下在整个Hostun砂样品中的空间和时间分布的研究。因此,我们首先考虑了三个不同的标准,为三个选定的织物变量校准了最小代表性元素尺寸。通过将元素以规则网格分布在试样上,我们能够根据空隙率、配位数和接触织物各向异性清楚地识别定位的开始。在空间和时间上,接触织物变量先于空隙率变化,因为它们对微小变化更敏感。图形摘要

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