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Quantitative Characterization of 3D Pore Structure in Porous Limestone

机译:多孔石灰岩3D孔隙结构的定量表征

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The pore structure in intact and inelastically deformed Indiana limestone have been studied using x-ray microtomography imaging. Guided by detailed microstructural observations and using Multi-level Otsu's thresholding method, the 3D images acquired at voxel side length of 4 μm were segmented into three domains: solid grains, macropores and an intermediate zone dominated by microporosity. Local Porosity can be defined to infer the porosity of each voxel. The macropores were individually identified by morphological processing and their shape quantified by their sphericity and equivalent diameter. With this segmentation, we obtained statistics on macropores on intact and deformed Indiana limestone which shows that inelastic compaction was followed by a significant reduction in the number of macropores. And also our results revealed the great potentiality to produce a quantitative analysis on porous material with the aid of micro CT images.
机译:使用X射线显微镜显像已经研究了完整和含有内印第安纳石灰石的孔结构。通过详细的微观结构观测和使用多级OTSU的阈值化方法,将血素侧长度施加4μm的3D图像分段为三个域:固体颗粒,大孔和由微孔占据的中间区。可以定义局部孔隙率以推断每个体素的孔隙率。通过形态学处理单独鉴定大孔,其形状通过它们的球形和等同的直径量化。通过这种分割,我们在完整和变形的印第安纳州石灰石上获得了巨大的统计,表明无弹性压实随后是大孔数量的显着降低。而且我们的结果揭示了借助于微型CT图像对多孔材料产生定量分析的巨大潜力。

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