Abstract

Damage to the internal structure of expansive soil under dry–wet cycles is the key factor for engineering damage to expansive soil. The expansive soil in Nanyang, Henan Province, China, is taken as the research object, and the damage characteristics of the internal structure of the expansive soil under dry–wet cycles are discussed. Computed Tomography (CT) images of the internal cracks of the expansive soil after zero to eight dry–wet cycles under different initial moisture contents were obtained using a CT machine, and the development of the internal structural cracks of the expansive soil was analyzed. The damage variable of the expansive soil defined by the ME value of CT and the relation between the damage variable, the number of dry–wet cycles, and the initial control moisture content are described. An empirical nonlinear damage model of the internal structure of expansive soil is established. Finally, the rationality of defining the damage variable by the ME value of CT is verified by the test results of the low-stress shear strength of the expansive soil. The results show that the first to fourth dry–wet cycles have great influence on the microstructure of the expansive soil and that internal microcracks are noticeably developed. With the increase in dry–wet cycles, the SD value increases gradually, and the anisotropy of the expansive soil becomes more significant. The dry–wet cycles result in the weakening of the connection between the particles of the expansive soil and in the damage of the internal structure, which is a nonlinear cumulative process. The ME value can be used to describe the damage evolution characteristics of expansive soil after dry–wet cycles.

Highlights

  • Expansive soil is a kind of water-sensitive material mainly composed of strong hydrophilic clay minerals

  • In a climate environment with frequent alternation of dry–wet conditions, the change in its internal moisture content causes the recurrence of expansion and contraction deformation of expansive soil

  • To better reflect the development of the internal cracks of expansive soil—that is, the longitudinal cracks, the longitudinal cracks obliquely intersecting with the sample, and the transverse cracks—the weighted average Computed Tomography (CT) numbers (ME values and SD values of variance) of three sections of each expansive soil sample are obtained as the representative values of the sample

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Summary

INTRODUCTION

Expansive soil is a kind of water-sensitive material mainly composed of strong hydrophilic clay minerals (montmorillonite and illite). In a climate environment with frequent alternation of dry–wet conditions, the change in its internal moisture content causes the recurrence of expansion and contraction deformation of expansive soil.. In a climate environment with frequent alternation of dry–wet conditions, the change in its internal moisture content causes the recurrence of expansion and contraction deformation of expansive soil.2,3 This kind of property will cause damage after excavation of the expansive soil slope and filling of the expansive soil subgrade. Shi et al. studied the effect of damage location and degree on the mechanical properties of expansive soil samples under stresses of 50 and 100 kPa by using triaxial shear tests and computed tomography (CT) technology. The content of this study will deepen the understanding of the development of damage to the internal structure of expansive soil under dry–wet cycles and promote the development of the damage theory of unsaturated soil

Expansive soil sample
Setting the initial moisture content
Sample preparation
CT test
Evolution of internal structural cracks
CT test results
Defining the damage degree variable
The relation of the damage variable with the number of dry–wet cycles
The relation of the damage variable with initial moisture content
RATIONALITY ANALYSIS OF DAMAGE DEFINED BY THE ME VALUE
CONCLUSIONS
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