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Title: The stress–strain behaviour and critical state parameters of an unsaturated granular fill material under different suctions
Authors: Liu, K 
Yin, JH 
Chen, WB 
Feng, WQ
Zhou, C 
Issue Date: Dec-2020
Source: Acta geotechnica, Dec. 2020, v. 15, no. 12, p. 3383-3398
Abstract: In mountainous western China, a large number of granular materials are used as construction materials in high-fill embankments. These granular fill materials in the embankments are typically unsaturated owing to the arid and semi-arid climates in this area. However, previous studies on unsaturated soils primarily focus on fine-grained soils. In this study, a series of triaxial tests were performed to determine the critical state parameters of a granular fill material in q–p¯, v–ln p¯, and vw–ln p¯ planes. An upgraded double-cell triaxial system (DCTS) was used in net confining pressures ranging from 0 to 450 kPa and matric suctions ranging from 0 to 160 kPa. This study demonstrates the good performance of the upgraded DCTS in unsaturated soil testing. Experimental results show that the critical state lines are almost parallel to those of saturated soil in the q–p¯ plane, suggesting that the friction angle is independent of suction. The total cohesion and hence the shear strength increase with suction. In the v–ln p¯ plane, both the intercept and slope of the critical state line increase with suction. Finally, it is observed that the intercept and slope decrease with increasing suction in the vw–ln p¯ plane.
Keywords: Critical state
High-fill embankment
Stress–strain
Suction
Unsaturated soil
Water retention curve
Publisher: Springer
Journal: Acta geotechnica 
ISSN: 1861-1125
EISSN: 1861-1133
DOI: 10.1007/s11440-020-00973-1
Rights: © Springer-Verlag GmbH Germany, part of Springer Nature 2020
This version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature’s AM terms of use(https://www.springernature.com/gp/open-research/policies/accepted-manuscript-terms), but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: http://dx.doi.org/10.1007/s11440-020-00973-1.
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