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基于热-力耦合的层状微裂纹岩体力学特性研究。

Study on mechanical properties of interbedded rock masses with microcrack based on thermal-mechanical coupling.

机构信息

College of Civil Engineering and Architecture, Xinjiang University, Urumqi, China.

Xinjiang Civil Engineering Technology Research Center, Urumqi, China.

出版信息

PLoS One. 2024 Feb 23;19(2):e0280486. doi: 10.1371/journal.pone.0280486. eCollection 2024.

Abstract

The mechanical properties of deep rock masses are significantly influenced by temperature and other factors. The effect of temperature on the strength of deep rock masses will pose a serious challenge to deep resource exploitation and engineering construction. In this paper, the thermal-mechanical coupling calculation model is established by particle flow code (PFC2D) to study the uniaxial compression response of rock masses with microcracks after temperature load. The strength of failure, microcracks, and strain was analyzed. The results show that: (i) When the soft rock thickness ratio Hs/H < 0.5, the displacement caused by the applied temperature is concentrated at the structural plane, and the contact force is concentrated at the end of the initial microcrack. When Hs/H ≥ 0.5, the displacement caused by the applied temperature is concentrated on both sides of the initial microcrack, and the contact force is concentrated in the hard rock area. (ii) The number of microcracks decreases with the increase of soft rock thickness under different working conditions. When the soft rock thickness ratio Hs/H < 0.5, the relationship curve between the number of microcracks and the vertical strain shows two stages of change. When Hs/H ≥ 0.5, the relationship curve between the number of cracks and the vertical strain changes shows three stages of change. (iii) When the soft rock thickness ratio Hs/H < 0.5, the failure strength decreases with the increase of soft rock thickness ratio at T = 100°C and 200°C. When T = 300°C and 400°C, the failure strength decreased first and then increased. When Hs/H ≥ 0.5, the failure strength increases with the increase of soft rock thickness at T = 200°C, 300°C, and 400°C. At T = 100°C, the failure strength decreases with the increase of soft rock thickness.

摘要

深部岩体的力学性质受温度等因素的影响显著。温度对深部岩体强度的影响将对深部资源开发和工程建设构成严重挑战。本文采用颗粒流程序(PFC2D)建立热-力耦合计算模型,研究了温度荷载作用后含微裂纹的岩体单轴压缩响应。分析了破坏强度、微裂纹和应变。结果表明:(i)当软岩厚度比 Hs/H<0.5 时,施加温度引起的位移集中在结构面处,接触力集中在初始微裂纹的末端。当 Hs/H≥0.5 时,施加温度引起的位移集中在初始微裂纹的两侧,接触力集中在硬岩区域。(ii)在不同工况下,随着软岩厚度的增加,微裂纹数量减少。当软岩厚度比 Hs/H<0.5 时,微裂纹数量与垂直应变的关系曲线呈现两个阶段的变化。当 Hs/H≥0.5 时,微裂纹数量与垂直应变的关系曲线呈现三个阶段的变化。(iii)当软岩厚度比 Hs/H<0.5 时,在 T=100°C 和 200°C 时,破坏强度随软岩厚度比的增加而减小。在 T=300°C 和 400°C 时,破坏强度先减小后增大。当 Hs/H≥0.5 时,在 T=200°C、300°C 和 400°C 时,破坏强度随软岩厚度的增加而增大。在 T=100°C 时,破坏强度随软岩厚度的增加而减小。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1b92/10889856/3e346894605e/pone.0280486.g001.jpg

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