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Non-Destructive Visualization and Quantification of 3-D Microstructure of Granular Materials and Direct Numerical Simulations

机译:颗粒材料3-D微观结构的无损可视化和量化及直接数值模拟

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This paper summarizes the key concepts from the recent published work of the authors on using both neutron and X-ray imaging techniques to study partially saturated sand and water flow through compacted sand. The goal of the manuscript is to serve as a review paper building on discrete contributions from cited publications for geomechanics community as the topic is rather new and concepts are connected. For this study, neutron and micro-CT based X-ray imaging was performed at Helmholtz-Zentrum-Berlin (HZB) in Germany. Due to different attenuation characteristics of neutrons and X-rays to three phases (silica, air and water) of partially saturated sand, radiation based images provide unique but complementary information in a non-destructive fashion. Water phase is very precisely identified with neutron radiation based images, and sand (silica) phase is well identified with X-ray images. An automatic image registration technique is implemented to combine neutron and X-ray images in the same coordinates for a detailed quantitative evaluation of micro-structural features in three dimensions. In-situ imaging experiment of flow through compacted sand was performed based on the dual modality imaging concept. The initial 3-D pore geometry was obtained from dry compacted sand specimen by using X-ray. The water flow pattern was monitored by using time-lapsed neutron radiography and tomography after a target water injection step. The initial microstructure obtained with X-ray tomography is also used to perform direct numerical simulations. Experiments based on using neutron and X-ray imaging technique thus provide unique opportunity to characterize partially saturated sand and investigate multi-phase flow behavior through porous media. Direct numerical simulation based on realistic geometry can account for complex pore geometry including heterogeneity of the pore structure.
机译:本文总结了作者最近发表的有关使用中子和X射线成像技术研究部分饱和砂土和流经压实砂土的水流的关键概念。该手稿的目的是作为评论论文,以地质力学界引用的出版物的不同贡献为基础,因为该主题相当新,而且概念相互关联。对于这项研究,在德国的Helmholtz-Zentrum-Berlin(HZB)进行了基于中子和微CT的X射线成像。由于中子和X射线对部分饱和的沙子的三相(二氧化硅,空气和水)的衰减特性不同,基于辐射的图像以无损方式提供了独特但互补的信息。通过基于中子辐射的图像可以非常精确地识别出水相,而通过X射线图像可以很好地识别出沙(硅)相。实现了一种自动图像配准技术,以将中子和X射线图像合并在相同的坐标中,以便在三个维度上对微观结构特征进行详细的定量评估。基于双重模态成像概念进行了流经压实砂土的原位成像实验。最初的3-D孔隙几何形状是使用X射线从干燥的压实砂土样品中获得的。在目标注水步骤之后,通过使用延时中子射线照相和断层摄影术来监测水流模式。 X射线断层扫描获得的初始微观结构也用于执行直接数值模拟。因此,基于中子和X射线成像技术的实验提供了独特的机会来表征部分饱和的沙子,并研究通过多孔介质的多相流动行为。基于逼真的几何形状的直接数值模拟可以说明复杂的孔几何形状,包括孔结构的异质性。

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