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Journal ArticleDOI

Influence of Thermal and Mechanical Loading on Development of Microcracks in Granite

TLDR
In this article, the authors used fluorescent dye impregnation technique to detect microcracks in unheated and heat-treated Bukit Timah Granite and found that the amount of micro cracks generated was proportional to the heating temperature.
Abstract
Fire safety is one of the most important concerns in underground engineering projects. Exposure to high temperature can weaken rocks and potentially cause catastrophic failure of the rock mass, either during the fire, or after the fire. In this study, Brazilian tensile tests were conducted on unheated and heat-treated Bukit Timah Granite. The microcrack length distribution and orientation were then recorded and analyzed through the fluorescent dye impregnation technique. The amount of microcracks generated was found to be proportional to the heating temperature. However, other factors such as the mineralogy and the texture of the rock were also found to influence the length and orientation of the microcracks. The modal microcrack lengths of the specimens were found to be similar despite different thermal and mechanical treatments of the specimens, while the orientation of the microcracks was found to be influenced by the type of minerals. Besides the average grain size, another factor which played a key role in determining the microcrack characteristics is the size and shape of the individual mineral grains.

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Journal ArticleDOI

Fluid Overpressurization of Rock Fractures: Experimental Investigation and Analytical Modeling

TL;DR: In this paper, the authors conducted a series of triaxial shear-flow experiments on sawcut fractures in granite and showed that the fracture responses can be dissimilar under various fluid pressurization conditions.
Journal ArticleDOI

Real-Time Visual Analysis of the Microcracking Behavior of Thermally Damaged Granite Under Uniaxial Loading

TL;DR: In this paper, real-time computed tomography (CT) scanning was performed on thermally damaged granite subjected to compression loading to observe the evolution of spatial three-dimensional (3D) microcracks and planar two-dimensional micro-cracks.
Journal ArticleDOI

Thermal cycling effects on the dynamic behavior of granite and microstructural observations

TL;DR: In this article, the authors investigated the thermal cycling effects on the dynamic behavior of granite and described its microstructure, and they showed that the dynamic properties of the P-wave velocity, p-wave modulus, and dynamic compressive strength exponentially decrease as the number of thermal cycles increases.
References
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Journal ArticleDOI

Subcritical crack growth in geological materials

TL;DR: A review of the experimental data on subcritical crack growth in geological materials is presented in this article, where the main parameters describing subcritical cracking growth are the critical stress intensity factor Kc, the sub critical crack growth limit Ko, and the relationship between Ko and Kc.
Journal ArticleDOI

Unified Theory of Thermal Shock Fracture Initiation and Crack Propagation in Brittle Ceramics

TL;DR: In this article, a fracture-mechanical theory for crack propagation in brittle ceramics subjected to thermal shock is presented and the criteria of crack stability are derived for a brittle solid uniformly cooled with triaxially constrained external boundaries.
Journal ArticleDOI

The Brazilian Disc Test for Rock Mechanics Applications: Review and New Insights

TL;DR: In this paper, a linear elastic numerical model is constructed to study crack initiation in a 50mm-diameter Brazilian disc using FLAC3D, and the maximum tensile stress and tensile strain are both found to occur about 5 mm away from the two loading points along the compressed diameter of the disc, instead of at the center of a disc surface.
Journal ArticleDOI

Micromechanics of thermally induced cracking in three crustal rocks

TL;DR: In this paper, the authors developed a Fracture mechanics model to interpret thermal cracking in the Oak Hall limestone and found that the internal stresses due to thermal expansion anisotropy are relaxed by plastic flow in this relatively fine grained limestone.
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