Quantitative 3D imaging of partially saturated granular materials under uniaxial compression

Milatz, Marius ORCIDiD
Hüsener, Nicole
Andò, Edward
Viggiani, Gioacchino
Grabe, Jürgen

DOI: https://doi.org/10.1007/s11440-021-01315-5
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/11244
Milatz, Marius; Hüsener, Nicole; Andò, Edward; Viggiani, Gioacchino; Grabe, Jürgen, 2021: Quantitative 3D imaging of partially saturated granular materials under uniaxial compression. In: Acta Geotechnica, 16, 11, 3573-3600, DOI: https://doi.org/10.1007/s11440-021-01315-5. 
 
Milatz, Marius; Institute of Geotechnical Engineering and Construction Management, Hamburg University of Technology (TUHH), Hamburg, Germany
Hüsener, Nicole; Institute of Geotechnical Engineering and Construction Management, Hamburg University of Technology (TUHH), Hamburg, Germany
Andò, Edward; Univ. Grenoble Alpes, Grenoble INP, CNRS, 3SR, Grenoble, France
Viggiani, Gioacchino; Univ. Grenoble Alpes, Grenoble INP, CNRS, 3SR, Grenoble, France
Grabe, Jürgen; Institute of Geotechnical Engineering and Construction Management, Hamburg University of Technology (TUHH), Hamburg, Germany

Abstract

Gauging the mechanical effect of partial saturation in granular materials is experimentally challenging due to the very low suctions resulting from large pores. To this end, a uniaxial (zero radial stress) compression test may be preferable to a triaxial one where confining pressure and membrane effects may erase the contribution of this small suction; however, volume changes are challenging to measure. This work resolves this limitation by using X-ray imaging during in situ uniaxial compression tests on Hamburg Sand and glass beads at three different initial water contents, allowing a suction-dependent dilation to be brought to the light. The acquired tomography volumes also allow the development of air–water and solid–water interfacial areas, water clusters and local strain fields to be measured at the grain scale. These measurements are used to characterise pertinent micro-scale quantities during shearing and to relate them to the measured macroscopic response. The new and well-controlled data acquired during this experimental campaign are hopefully a useful contribution to the modelling efforts—to this end they are shared with the community.

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