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耦合水热作用对典型砂岩断裂特性的影响

Influence of coupled water and thermal treatments on the fracture characteristics of a typical sandstone.

作者信息

Luo Yi, Zhong Haohong, Ren Li, Li Cunbao

机构信息

School of Environment and Civil Engineering, Dongguan University of Technology, Dongguan, 523808, China.

Guangdong Provincial Key Laboratory of Intelligent Disaster Prevention and Emergency Technologies for Urban Lifeline Engineering, Dongguan, 523808, China.

出版信息

Sci Rep. 2024 May 17;14(1):11324. doi: 10.1038/s41598-024-62025-y.

Abstract

Understanding the fracture behavior of rock after coupled water and thermal environment is important for many geotechnical projects. This study examines the influence of coupled water and thermal treatments on the fracture toughness and characteristics of a typical sandstone under mode I and mode II loading conditions. Notched deep beam (NDB) specimens were utilized and subjected to soaking treatments at various water temperatures (23 °C, 60 °C, and 99 °C). The experimental results indicate a significant reduction in both mode I and mode II fracture toughness values, with reductions ranging from 15.4% to 13.2% for mode I and 26.1% to 8.9% for mode II respectively. As the water temperatures increase, a slightly rising trend is observed in both mode I and mode II fracture toughness within the examined temperature range. Sandstone specimens displayed typical brittle fracture characteristics at lower soaking temperatures. For mode I specimens, an increase in ductility was evident with higher soaking temperatures, while the ductile behavior is less pronounced in the mode II specimens. Based on the Maximum Tangential Stress (MTS) criterion and the Generalized Maximum Tangential Stress (GMTS) criterion, the predicted values of mode II fracture toughness and the fracture process zone (FPZ) were discussed. The results show that both the GMTS and MTS criteria exhibit inaccuracies in predicting the mode II fracture toughness of sandstone treated at different soaking water temperatures. However, the GMTS criterion, which incorporates T-stress, demonstrates smaller errors compared to the MTS criterion. The study shows that the radius r of the fracture process zone is not a constant under both mode I and mode II loading conditions. The calculation of the fracture process zone radius r in the GMTS criterion requires further theoretical and experimental study.

摘要

了解岩石在水热耦合环境后的断裂行为对许多岩土工程至关重要。本研究考察了水热耦合处理对典型砂岩在I型和II型加载条件下断裂韧性及特性的影响。采用切口深梁(NDB)试样,并在不同水温(23℃、60℃和99℃)下进行浸泡处理。实验结果表明,I型和II型断裂韧性值均显著降低,I型的降低幅度为15.4%至13.2%,II型的降低幅度为26.1%至8.9%。随着水温升高,在所考察的温度范围内,I型和II型断裂韧性均呈现出略有上升的趋势。砂岩试样在较低浸泡温度下表现出典型的脆性断裂特征。对于I型试样,浸泡温度越高,延性增加越明显,而II型试样中的延性行为则不太明显。基于最大切向应力(MTS)准则和广义最大切向应力(GMTS)准则,讨论了II型断裂韧性和断裂过程区(FPZ)的预测值。结果表明,GMTS和MTS准则在预测不同浸泡水温处理的砂岩的II型断裂韧性时均存在不准确之处。然而,考虑T应力的GMTS准则与MTS准则相比,误差较小。研究表明,在I型和II型加载条件下,断裂过程区半径r都不是一个常数。GMTS准则中断裂过程区半径r的计算需要进一步的理论和实验研究。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7418/11101422/9ef0e1aa7889/41598_2024_62025_Fig1_HTML.jpg

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