评估热处理、单轴加载注浆非持续性中硬岩石的断裂力学:数字图像相关和FracPaQ分析

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Gaurav Kumar Mathur, Arvind Kumar Jha, Gaurav Tiwari
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引用次数: 0

摘要

热载荷、开挖和地震波速度等因素对岩石节理的动载荷进一步加剧了其敏感性。使用适当的技术来恢复这些岩体的强度,以提高边坡和隧道的稳定性,减轻未来的痛苦和损害,这是至关重要的。本研究探讨了单轴加载对非持久岩体在100 ~ 400℃温度下峰值强度和断裂扩展行为的影响。这些参数已经在有接缝的样品中进行了检测(即,由牙石膏(DP)制成,接缝与样品中间的水平方向倾斜30°),并使用(i)水泥,(ii)砂-水泥砂浆(1:3的比例)和生物混凝土(SCB)混合物填充浆液,以及(iii)环氧树脂。结果表明,注浆可以缓解任何岩体中存在的缺陷。未经热处理的环氧灌浆比水泥和SCB混合灌浆更有效。该研究还清楚地描述了温度变化对未灌浆和灌浆试件强度行为的影响。未灌浆、SCB混合料、水泥和环氧灌浆试样的应变场变化范围分别为0.01 ~ 0.25、0.05 ~ 0.55、0.02 ~ 0.14和0.01 ~ 0.1。在未灌浆的试样中,应变随着热处理的增加而增加,从拉伸破坏模式过渡到远场破坏模式。灌浆后,观察到应变增加。在以SCB混合料灌浆的试样中,在250°C以下,剪切裂纹占主导地位,之后出现远场裂纹。在水泥灌浆试样中,远场裂纹在200°C时被观察到,随后过渡到拉伸破坏模式。然而,环氧灌浆试样的远场破坏模式从热处理开始,从100°C开始。通过数字图像相关(DIC)和FracPaQ分析对未灌浆和灌浆试件的裂纹扩展进行了详细观察。DIC技术可以精确测量应变分布和变形,而FracPaQ可以提供详细的裂缝网络和方向分析。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Assessing fracture mechanics in thermally treated, uniaxial loaded grouted non-persistent medium-hard rock: a digital image correlation and FracPaQ analysis

Assessing fracture mechanics in thermally treated, uniaxial loaded grouted non-persistent medium-hard rock: a digital image correlation and FracPaQ analysis

Dynamic loading along the rock joints from factors such as thermal loads, excavation, and seismic wave velocity further exacerbates susceptibility. It is crucial to restore the strength of such rock masses using appropriate techniques to enhance the stability of slopes and tunnels and mitigate future distress and damage. This study investigates the impact of uniaxial loading on the peak strength and fracture propagation behaviour of non-persistent rock masses subjected to temperatures from 100 °C to 400 °C. These parameters have been examined in jointed samples (i.e., prepared by dental plaster (DP) with joint at 30° inclinations to the horizontal in the middle of the specimen) and filled with grouts using (i) cement, (ii) sand-cement mortar (in a 1:3 ratio) and bio-concrete (SCB) mix, and (iii) epoxy resin. The results reveal that grouting can mitigate the presence of defects in any rock mass. Without heat-treated specimens with epoxy grout are more effective than those with cement and SCB mix grout. The study also clearly delineates the effects of temperature variation on the strength behaviour of both un-grouted and grouted specimens. The strain field of samples without subjected to heat treatment varies from 0.01 to 0.25, 0.05 to 0.55, 0.02 to 0.14 and 0.01 to 0.1 in un-grouted, SCB mix, cement and epoxy grouted, respectively. In un-grouted specimens, strain increases with higher thermal treatments, transitioning from tensile to far-field failure modes. When grouting is introduced, an increase in strain is observed. In specimens grouted with SCB mix, shear cracks dominate up to 250 °C, after which far-field cracks appear. In cement-grouted specimens, far-field cracks are observed up to 200 °C, followed by a transition to tensile failure mode. However, far-field failure mode in epoxy grouted specimens initiates from the onset of thermal treatments, starting at 100 °C. The detailed observations on crack propagation along un-grouted and grouted specimens is made via Digital Image Correlation (DIC) and FracPaQ analysis. The DIC technique enables precise measurement of strain distribution and deformation, while FracPaQ provides detailed analysis of fracture networks and orientations.

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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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