Abstract

Shear strength of shallow expansive soil varies along with the depth under the freeze-thaw effect. This work investigates shear strength characteristics of shallow expansive soil by simulating the actual freeze boundary conditions of seasonal frozen areas with water supplement. An integrated approach incorporating the freeze-thaw test and direct shear test was adopted. Firstly, unidirectional freezing tests for expansive soil columns under three different freezing temperature gradients were carried out. Secondly, direct shear tests under low vertical stress were performed on the standard samples, which were prepared by using cutting rings cut the thawed expansive soil columns into nine segments along with the depth. Temperature, water content, and dry density at different depths were also investigated after the freeze-thaw process. The test results showed that, after the freeze-thaw process, the shear strength of expansive soil columns showed significant differences along with the depth and highly correlated with water content, specifically the higher water content and the lower shear strength. The minimum shear strength in the expansive soil columns occurred at the soil layer below the frozen and unfrozen zones interface. The expansive soil column’s shear strength changed most under the moderate freezing temperature gradient corresponding to the most considerable shear strength reduction. Moreover, the significant decrease in cohesion was the main reason for the shear strength reduction of expansive soil after the freeze-thaw process. These results indicate significant depth variability in shear strength of expansive soil under the freeze-thaw effect.

Highlights

  • Expansive soil is a highly plastic soil with many hydrophilic clay minerals like montmorillonite and illite

  • All the expansive soil columns were divided into the frozen zone and unfrozen zone according to the freezing point of −1.64°C, considering the thickness of the frozen fringe is very small, usually ranging from 1.5 mm to 8 mm [26, 27]

  • Relationship between Shear Strength and Frozen Characteristics. e minimum shear strength in the expansive soil columns occurred at the soil layer below the frozen and unfrozen zone interface. e reduction of shear strength is attributed to the soil structure damage during the freezing process [28]. e formation of irregular pores and large cracks due to water migration and water phase change in soil particles and pores is the main reason for soil structure damage [29,30,31]. e more significant the water migration, the more the considerable changes in the soil structure, which induce more significant degradation of soil shear strength. e inhomogeneity of shear strength along depth is consistent with that of water content along with the depth

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Summary

Introduction

Expansive soil is a highly plastic soil with many hydrophilic clay minerals like montmorillonite and illite. 380 km expansive soil open channel in the middle route of South-to-North Water Transfer Project (SNWTP) and more than 260 km of expansive soil cutting slope in the Jilin-Tumen-Hunchun high-speed railway in China were both located in seasonal frozen regions [4,5,6]. In these hydraulic engineering and traffic engineering projects, slope instability of expansive soil frequently occurs after the freeze-thaw process. Expansive soil’s shear strength under the freeze-thaw effect is the necessary mechanical parameter

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