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首页> 外文期刊>Journal of geotechnical and geoenvironmental engineering >Capillary Suction Measurements in Granular Materials and Direct Numerical Simulations Using X-Ray Computed Tomography Microstructure
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Capillary Suction Measurements in Granular Materials and Direct Numerical Simulations Using X-Ray Computed Tomography Microstructure

机译:颗粒材料中的毛细管吸力测量和使用X射线计算机断层扫描微结构的直接数值模拟

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摘要

Because of the recent advancements in hardware and reconstruction algorithms, multiphase flow modeling in porous media is experiencing a shift toward using advanced imaging techniques such as X-ray computed tomography in conjunction with direct numerical simulations. This approach captures heterogeneities in soil samples utilized in laboratory testing and results in quick and less tedious predictions compared to the existing methods. In this paper, an experimental setup is developed specifically to validate numerical predictions of the soil water retention curve (SWRC) for two types of sands with identical size but distinct grain morphology of round (Ottawa sand) and angular particle shape (Q-Rok). The complex 3D pore network is captured noninvasively using high-resolution attenuation-based X-ray computed tomography. The numerical predictions are carried out by solving a Young-Laplace equation using the pore morphology method. The experimental results and numerical predictions match well, including the effect of hysteresis in SWRC measurements. The spatial distribution of pore water and pore air corresponding to different capillary suctions is obtained from numerical predictions, providing greater insights into the hydromechanical behavior of partially saturated soils. The sensitivity of the voxel size on simulations is quantified by predicting the pore size distribution of Ottawa sand at three different tomography resolutions.
机译:由于硬件和重建算法的最新进展,多孔介质中的多相流建模正朝着使用先进的成像技术(例如X射线计算机断层扫描)与直接数值模拟相结合的方向发展。与现有方法相比,该方法可捕获实验室测试中所用土壤样品中的异质性,并能进行快速而又乏味的预测。在本文中,专门开发了一种实验装置,以验证两种类型的沙子(大小相同,但颗粒形态分别为圆形(渥太华)和角形颗粒(Q-Rok))的土壤保水曲线(SWRC)的数值预测。使用高分辨率的基于衰减的X射线计算机断层扫描,无创地捕获复杂的3D孔网络。通过使用孔隙形态学方法求解Young-Laplace方程进行数值预测。实验结果和数值预测非常吻合,包括SWRC测量中的磁滞效应。孔隙水和孔隙空气的空间分布与不同的毛细吸力相对应,这是通过数值预测获得的,从而可以更好地了解部分饱和土壤的水力力学行为。通过预测三种不同的层析成像分辨率下渥太华砂的孔径分布,可以量化模拟中体素尺寸的敏感性。

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