Journal
JOURNAL OF ROCK MECHANICS AND GEOTECHNICAL ENGINEERING
Volume 14, Issue 6, Pages 1710-1721Publisher
SCIENCE PRESS
DOI: 10.1016/j.jrmge.2022.02.010
Keywords
High temperature; Confining pressure; Thermo-mechanical (TM) damage; Thermal damage; Mechanical damage
Categories
Funding
- Bowen Basin Underground Geotechnical Society
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The severity of underground rock dynamic disasters is increasing due to the deepening of human operations underground. Understanding the thermo-mechanical behavior of rocks is important for the long-term safety and maintenance of underground tunnels and mining. This study proposed a statistical coupled thermo-mechanical constitutive model for sandstone under high temperature and pressure conditions, and validated the model using triaxial test results. The model showed good agreement with the experimental results up to 600 degrees C.
Underground rock dynamic disasters are becoming more severe due to the increasing depth of human operations underground. Underground temperature and pressure conditions contribute significantly to these disasters. Therefore, it is important to understand the coupled thermo-mechanical (TM) behaviour of rocks for the long-term safety and maintenance of underground tunnelling and mining. Moreover, investigation of the damage, strength and failure characteristics of rocks under triaxial stress conditions is important to avoid underground rock disasters. In this study, based on Weibull distribution and Lemaitre's strain equivalent principle, a statistical coupled TM constitutive model for sandstone was established under high temperature and pressure conditions. The triaxial test results of sandstone under different temperature and pressure conditions were used to validate the model. The proposed model was in good agreement with the experimental results up to 600 degrees C. The total TM damage was decreased with increasing temperature, while it was increased with increasing confining pressure. The model's parameters can be calculated using conventional laboratory test results. (C) 2022 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
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