Abstract

Natural aeolian sand has the characteristics of low cohesion and poor water stability. In order to improve its crack resistance properties in the process of freeze-thaw cycles, P.O 42.5 ordinary Portland cement was added to form a mixture called cement improved aeolian sand (CIAS). SEM was used to analyze the microscopic micro-structure of CIAS at different times (7 days and 28 days). The mechanical properties of CIAS samples affected by freeze-thaw cycles were tested in a triaxial instrument, and gray-scale images of the three-phase distribution in the CIAS after freeze-thaw cycling were obtained by computed tomography (CT) scanning technology. The pore characteristic parameters (pore area, fractal dimension, and crack length) were studied by digital image process technique. Based on classical Griffith fracture theory, the development of the crack length and crack width with increasing freeze-thaw cycles is determined. Assuming that the pore area subordinates to the Weibull distribution, the parameters of the Weibull distribution, the damage evolution defined by the elastic modulus attenuation, and the pore area development of CIAS were determined. Research shows the cohesion decreases and internal friction angle increases with increasing cycle numbers. Three development patterns are observed: crack growth, crack closure, and crack merging, and the three patterns interact during freeze-thaw cycling. Furthermore, the fractal dimension of the pore edge fluctuates with the increasing number of freeze-thaw cycles. This work provides a theoretical basis for the application of aeolian sand and develops a method for disaster prevention in applications of freeze-thaw cycling.

Highlights

  • Aeolian sand is a natural granular medium that is universally distributed in the northwestern and northeastern regions of China, such as the Shanxi province and inner Mongolia

  • Consolidated undrained (CU) shear tests of cement improved aeolian sand (CIAS) were carried out after freeze-thaw cycling under the confining pressures of 50, 100, and 200 kPa

  • Due to the closed nature of the system during the freezing state, the moisture in the CIAS samples gradually migrates to the cold peak surface outside of the sample, at which point ice crystals precipitate on the surface of the sample

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Summary

Introduction

Aeolian sand is a natural granular medium that is universally distributed in the northwestern and northeastern regions of China, such as the Shanxi province and inner Mongolia This particular material originates from the weathering of rocks and is formed by wind transport. The mechanical properties of soils after freeze-thaw cycling are directly related to the engineering performance of geotechnical structures such as the bearing capacity of foundations and the sliding resistance force in artificial and natural slopes [4,5,6]. Based on fact that the addition of siliceous fly ashes into the concrete can improve its fracture toughness and decrease the crack width [23,24], to analyze the evolutionary characteristics of pores and fractures, CT scanning and IPP (Image-Pro Plus) image processing technology can be used to analyze the damage evolution laws of CIAS after freeze-thaw cycling. This study is expected to offer a basis for disaster prevention and the control of freeze-thaw-resistant CIAS road base in the future

Materials
Experimental Design
Effect of Freeze-Thaw Cycles on Physical Properties
Effect of Freeze-Thaw Cycles on Shear Strength
Triaxial shear teststests of samples treated with different freeze-thaw
CT Scanning of Pore Evolution
Analysis of Light Intensity after Freeze-Thaw Cycling
Trend of Fractal Dimensions of Pore Evolution
15. Variation
Evolution
Figure
Statistical Distribution of Pore Area
20. Distribution
Evolution of Freeze-Thaw Damage
N 1 N ef A0
E N E0 1
Conclusions
Full Text
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