Abstract

The lateral unloading strength and deformation of surrounding frozen rock are the key parameters for safety evaluation of frozen shaft construction. A low-temperature and high-pressure rock triaxial test system was used to simulate freezing construction, and a constant axial pressure unloading confining pressure test was carried out on frozen sandstone. The effects of freezing temperature, initial confining pressure, and unloading rate on the strength, deformation, and failure modes of frozen sandstone are studied. The main results of the study are as follows: (1) under the initial confining pressure of 20 MPa, the temperature of the sandstone decreases from 20°C to –5°C, and the peak stress and elastic modulus of triaxial compression increase by approximately 3 times. Under lateral unloading conditions, the peak stress of frozen sandstone is about 2∼3 times that of 20°C sandstone, and the peak strain of 20°C sandstone is smaller than that of frozen sandstone. The temperature of frozen sandstone decreases and the rate of increase in the peak stress of triaxial compression is slightly less than the rate of increase in the peak stress of lateral unloading. (2) The initial confining pressure of frozen sandstone increases, the growth rate of axial and radial strain increases, the radial strain dominates the failure process, and the lateral unloading strength decreases significantly. (3) The lateral unloading rate of frozen sandstone increases, the peak strength increases, and the axial and radial strain decrease. At a low unloading rate, partial creep deformation occurs. (4) The frozen rock sample undergoes tensile splitting failure under lateral unloading. According to the stress-strain curve of the frozen rock sample, the relationship between changes in the deformation modulus and changes in the confining pressure unloading amount during the unloading process of the rock sample is obtained.

Highlights

  • When mining deep coal resources, the artificial freezing method is often used to cross deep water-rich soft rock strata. e freezing of the shaft wall can block the leakage of groundwater, provide a watertight working environment, and improve the strength and deformation resistance of the excavated rock and soil [1]

  • With the development of artificial freezing construction technology and cold area engineering, useful results have been achieved in research related to the mechanical properties of frozen rock. e unfrozen water content of saturated rock decreases with the decrease of freezing temperature, which has a great influence on the strength and deformation [2]

  • As the freezing temperature decreases, the axial and radial strains decrease, and the rate at which peak stress increases in triaxial compression is slightly lower than the rate of peak stress increase in lateral unloading

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Summary

Introduction

When mining deep coal resources, the artificial freezing method is often used to cross deep water-rich soft rock strata. e freezing of the shaft wall can block the leakage of groundwater, provide a watertight working environment, and improve the strength and deformation resistance of the excavated rock and soil [1]. Temperature has a substantial influence on the mechanical behavior of rock and soil. Excavating a frozen shaft is equivalent to lateral unloading of frozen rock. Studying the mechanical characteristics of frozen rock lateral unloading is very important to the construction design of the frozen shaft. With the development of artificial freezing construction technology and cold area engineering, useful results have been achieved in research related to the mechanical properties of frozen rock. E unfrozen water content of saturated rock decreases with the decrease of freezing temperature, which has a great influence on the strength and deformation [2]. Kodama et al [5] concluded that the strength of water-containing rock is inversely proportional to temperature. Gao et al [6] concluded that the average fracture toughness of frozen sandstone was 10.47% ∼ 158.33% higher than that of normal temperature

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