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Microstructural analysis of unsaturated granular soils using X-ray computed tomography.

机译:X射线计算机体层摄影术对非饱和颗粒状土壤的微观结构分析。

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摘要

This study presents microstructural characterization of partially saturated granular soils using X-ray computed tomography (CT). In the funicular and pendular saturation regimes of unsaturated soils, pore-water assumes a complex fabric consisting of saturated pockets of water under negative pressure and a network of liquid bridges. Characterization of this complex fabric is essential to the development of effective stress relationship for partially saturated soils.;A novel experimental setup for real time monitoring of microstructure inside an X-ray computed tomography system is designed with modifications to the Tempe type cell and hanging water column method. The experimental apparatuses are integrated with X-ray CT scanner to generate three dimensional images of partially saturated soil microstructure under controlled saturation direction and suction.;Analytical approaches are combined with digital image processing techniques to quantify microstructural parameters of interest. Algorithms and macros are developed to quantify the degree of saturation and the fabric tensor of the liquid phase from X-ray CT images. A standalone image processing program is developed as an integral part of the scanning and image pre-processing routines.;A new formulation for effective stress in partially saturated soil is developed based on virtual work principles incorporating explicitly a tensor measure that characterizes the complex fabric resulting from saturated pockets and networks of liquid bridges. When the soil becomes fully saturated, the formulation reduces to the Terzaghi's effective stress.;The fabric tensor of the liquid phase, however, is observed to vary throughout the saturation and desaturation processes. It is therefore essential that the new formulation, coupled with the experimental methods proposed here, is needed to fully describe the effective stress in partially saturated soils.
机译:这项研究提出了使用X射线计算机断层扫描(CT)对部分饱和的颗粒状土壤进行微观结构表征。在非饱和土壤的缆索状和摆动状饱和状态下,孔隙水呈现出一种复杂的结构,该结构由负压下的饱和水囊和液桥网络组成。这种复杂织物的特性对于开发部分饱和土壤的有效应力关系至关重要。通过对Tempe型单元和悬挂水的修改,设计了一种新颖的实验装置,用于实时监测X射线计算机断层摄影系统内部的微观结构列方法。实验装置与X射线CT扫描仪集成在一起,在受控的饱和方向和吸力下生成部分饱和土壤微观结构的三维图像。分析方法与数字图像处理技术相结合,以量化感兴趣的微观结构参数。开发了算法和宏来量化X射线CT图像的饱和度和液相的织物张量。开发了一个独立的图像处理程序,作为扫描和图像预处理程序的组成部分。;基于虚拟工作原理,开发了一种针对部分饱和土壤中有效应力的新公式,该原理明确结合了张量度量,以表征复杂的织物结果。来自饱和的囊袋和液桥网络。当土壤完全饱和时,配方会降低到Terzaghi的有效应力。然而,观察到液相的织物张量会在整个饱和和去饱和过程中变化。因此,至关重要的是,需要使用新的配方以及此处提出的实验方法来全面描述部分饱和土壤中的有效应力。

著录项

  • 作者

    Manahiloh, Kalehiwot Nega.;

  • 作者单位

    Washington State University.;

  • 授予单位 Washington State University.;
  • 学科 Engineering Civil.
  • 学位 Ph.D.
  • 年度 2013
  • 页码 169 p.
  • 总页数 169
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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