Abstract

The artificial fracturing technique under coupled hydro-mechanical effects is widely used in many rock engineering. Therefore, the study on the fracturing behaviors and mechanical properties of hydro-mechanical coupled cracks is very crucial. In this study, a series of fracturing tests were conducted on the cylinder gypsum specimens with single pre-existing cracks using triaxial compression loading system. Water pressure was applied inside the pre-existing cracks and led to the specimen failure with external compression loading. A new type of cracks, namely horizontal coupled cracks (HCC), were found in some specimens. Macroscopic observations reveal that HCC, which were mainly caused by the hydraulic pressure, were different from any tensile wing cracks, shear secondary cracks, or shear anti-wing cracks. Subsequently, a microscopic study was performed using scanning electron microscope (SEM), the outcomes suggest that: (1) Shear fracturing zones (SFZ) and tensile fracturing zones (TFZ) under coupled hydro-mechanical effects displayed distinct characteristics on orientations, length, and independence of gypsum grains; and (2) the HCC were tensile cracks when they just initiated from outer tips of pre-existing cracks. While tensile stress made major contribution to the specimen failure during the whole fracturing processes, the HCC became tensile and shear mixed cracks when the specimen was about to fail.

Highlights

  • Crack fracturing under coupled hydro-mechanical effects is a widely used method for creating cracks in deep rock formation and enhancing hydraulic conductivity of geological reservoirs.Despite this important technique, it is routinely adopted in oil and gas extraction and enhanced geothermal systems, the fracturing behaviors, and mechanical properties of hydro-mechanical coupled cracks are not comprehensively understood [1]

  • Microscopic investigations were conducted on scanning pieces cut from the horizontal coupled cracks (HCC)

  • Several conclusions are obtained from the macroscopic observation and microscopic analysis in the present study

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Summary

Introduction

Crack fracturing under coupled hydro-mechanical effects is a widely used method for creating cracks in deep rock formation and enhancing hydraulic conductivity of geological reservoirs. Amalokwu et al [37] studied the effect of saturated cracks in synthetic rock specimens, the results showed that the presence of air-water cracks significantly influence the shear waves. Hydro-mechanical fracturing is an exceedingly complicated process, which is affected by many controllable or uncontrollable factors such as the mechanical properties of rock (strength, stiffness, saturation, porosity, and size of grains), the statuses of fracturing fluid (type, viscosity, temperature, and injection rate), external stress states, and geometry of pre-existing cracks. The fracturing behaviors and mechanical properties of coupled cracks in cylinder rock-like specimens are investigated and analyzed. Summaries and conclusions are provided towards the end of the paper

Specimen Preparation
Test Setup and Procedures
Photograph
Trajectories
Trajectories of Dryof
Microscopic Study
Shear and Tensile Fracturing Zones
Mechanical
A At andthe
Findings
Conclusions
Full Text
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