Abstract

Ice lens is the key factor which determines the frost heave in engineering construction in cold regions. At present, several theories have been proposed to describe the formation of ice lens. However, most of these theories analyzed the ice lens formation from a macroscopic view and ignored the influence of microscopic pore sizes and structures. Meanwhile, these theories lacked the support of measured data. To solve this problem, the microscopic crystallization stress was converted into the macro mean stress through the principle of statistics with the consideration of pore size distribution. The mean stress was treated as the driving force of the formation of ice lens and induced into the criterion of ice lens formation. The influence of pore structure and unfrozen water content on the mean stress was analyzed. The results indicate that the microcosmic crystallization pressure can be converted into the macro mean stress through the principle of statistics. Larger mean stress means the ice lens will be formed easier in the soil. The mean stress is positively correlated with initial water content. At the same temperature, an increase to both the initial water content and the number of pores can result in a larger mean stress. Under the same initial water content, mean stress increases with decreasing temperature. The result provides a theoretical basis for studying ice lens formation from the crystallization theory.

Highlights

  • IntroductionThese projects have promoted the research on frost heave

  • With the development of national defense and economic construction, an increasing number of foundation engineering projects have been built in cold regions in China, such as the Qinghai-TibetHighway, Qinghai-Tibet Railway, Qinghai-Tibet Transmission and Harbin-Dalian high speed railway [1,2,3]

  • Based on the microscopic crystallization theory, a theoretical model is developed for mechanical criterion of formation of ice lens considering the initial water content, temperature, pore radius and pore size distribution

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Summary

Introduction

These projects have promoted the research on frost heave. To simulate the formation of ice lens, many frost heave models including the criterion of ice lens formation have been proposed [7,8,9]. These criterions can be divided into two types: the thermal method and the mechanical method. These criterions of the mechanical method can be divided into four groups

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