X-Ray microtomography of mercury intruded compacted clay: An insight into the geometry of macropores
Shengyang Yuan, Xianfeng Liu, Yongxin Wang, Pierre Delage (NAVIER UMR, 8205), Patrick Aimedieu, Olivier Buzzi

TL;DR
This study uses X-ray microtomography to analyze the geometry of macropores in compacted clay, revealing insights into pore shape, distribution, and differences from mercury intrusion porosimetry results, enhancing understanding of soil microstructure.
Contribution
It introduces a combined approach of MIP and X-$t$T to characterize macropore geometry and distribution in compacted clay, highlighting limitations and differences of each method.
Findings
Macropores are evenly distributed and mostly non-spherical.
Large pore bodies with high aspect ratio are visible in X-$t$T.
Differences in pore size measurements are due to experimental protocols and pore geometry effects.
Abstract
Soil properties, such as wetting collapse behavior and permeability, are strongly correlated to the soil microstructure. To date, several techniques including mercury intrusion porosimetry (MIP), can be used to characterize the microstructure of soil, but all techniques have their own limitations. In this study, the features of mercury that penetrated and has been entrapped in the pore network of the specimens through MIP testing were investigated by X-Ray microtomography (X-CT), in order to give an insight into the geometry of macropores and possible ink-bottle geometry. Two conditions of water content and density were selected for the compacted Maryland clay. The distribution and geometry features of mercury entrapped in the microstructure after MIP were characterized and pore size distributions were also reconstructed. The results suggest that, for the two conditions studied in…
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