4.7 Article

Effects of Thermal Treatment on Tensile Strength of Laurentian Granite Using Brazilian Test

期刊

ROCK MECHANICS AND ROCK ENGINEERING
卷 48, 期 6, 页码 2213-2223

出版社

SPRINGER WIEN
DOI: 10.1007/s00603-015-0712-3

关键词

Laurentian granite; Dynamic tensile strength; Thermal treatment; Brazilian test; SHPB

资金

  1. National Natural Science Foundation of China [51304241]
  2. China Scholarship Council (CSC)

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The effect of thermal treatment on several physical properties and the tensile strength of Laurentian granite (LG) are measured in this study. Brazilian disc LG specimens are treated at temperatures of up to 850 A degrees C. The physical properties such as grain density, relative volume change per degree, and P-wave velocity are investigated under the effect of heat treatment. The results indicate that both the density and the P-wave velocity decrease with the increase in heating temperature. However, the relative volume change per degree is not sensitive below 450 A degrees C, while a remarkable increase appears from 450 to 850 A degrees C. All cases are explained by the increase in both number and width of the thermally induced microcracks with the heating temperature. Brazilian tests are carried out statically with an MTS hydraulic servo-control testing system and dynamically with a modified split Hopkinson pressure bar (SHPB) system to measure both static and dynamic tensile strength of LG. The relationship between the tensile strength and treatment temperatures shows that static tensile strength decreases with temperature while the dynamic tensile strength first increases and then decreases with a linear increase in the loading rate. However, the increase in dynamic tensile strength with treatment temperatures from 25 to 100 A degrees C is due to slight dilation of the grain boundaries as the initial thermal action, which leads to compaction of rock. When the treatment temperature rises above 450 A degrees C, the quartz phase transition results in increased size of microcracks due to the differential expansion between the quartz grains and other minerals, which is the main cause of the sharp reduction in tensile strength.

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