Abstract

Variation in the heating rate due to different geothermal gradients is a cause of much concern in underground rock engineering such as deep sea and underground tunnels, nuclear waste disposal, and deep mining. By using a split Hopkinson pressure bar (SHPB) and variable-speed heating furnace, the dynamic compressive properties of granite were obtained after treatments at different heating rates and temperatures; these properties mainly included the dynamic compressive strength, peak strain, and dynamic elastic modulus. The mechanism of heating rate action on the granite was simultaneously analyzed, and the macroscopic physical properties were discussed. The microscopic morphological features were obtained by scanning electron microscopy (SEM), and the crack propagation was determined by high-speed video camera. The experimental results show that the dynamic compressive strength and elastic modulus both show an obvious trend of a decrease with the increasing heating rate and temperature; the opposite phenomenon is observed for the peak strain. The relationships among the dynamic compressive properties and temperature could be described by the quadratic function. The ductility of granite is enhanced, and the number and size of cracks increase gradually when the heating rate and temperature increase. The microstructure of rock is weakened by the increased thermal stress, which finally affects the dynamic compressive properties of rock.

Highlights

  • In recent years, due to different geothermal gradients, it has been noticed that the heating rate is one of the significant factors that affect the mechanical properties of a rock mass in deep underground rock engineering such as deep sea and underground tunnels, nuclear waste disposal, and deep mining

  • The rock treated at a temperature of 25°C stands for that of untreated; that is, the rock is treated at the heating rate of 0°C/min

  • Conclusions regarding the dynamic compressive strength, peak strain, dynamic elastic modulus, and microstructural characteristics were drawn during the investigation and discussion

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Summary

Introduction

Due to different geothermal gradients, it has been noticed that the heating rate is one of the significant factors that affect the mechanical properties of a rock mass in deep underground rock engineering such as deep sea and underground tunnels, nuclear waste disposal, and deep mining. Deep rock masses simultaneously suffer from various complex and dangerous environments including high ground stress, high humidity, high temperature caused by high-heat injection, and strong dynamic disturbance generated by drilling or blasting [1,2,3]. This situation is very different from that of shallow rock masses.

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