Study on the damage mechanism and evolution model of preloaded sandstone subjected to freezing–thawing action based on the NMR technology

IF 3.6 4区 材料科学 Q2 MATERIALS SCIENCE, MULTIDISCIPLINARY Reviews on Advanced Materials Science Pub Date : 2024-07-03 DOI:10.1515/rams-2024-0034
Shuailong Lian, Wen Wan, Yanlin Zhao, Wenqing Peng, Can Du, Hao Hu
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Abstract

Investigating the damage degradation of rock during the freezing and thawing process is more consistent with the actual engineering environment, considering its internal initial damage. In this study, the effects of initial damage from preloading and subzero-temperature freezing–thawing on microscopic and macroscopic mechanical properties of sandstone were studied based on the nuclear magnetic resonance (NMR) technique. The results show that the P-wave velocity of the sample decreased, while the porosity increased as the initial damage level increased. The distribution of T2 signal intensity exposed to the low-temperature freezing–thawing–saturation treatment was rather larger than that under normal temperature conditions for samples with different levels of initial damage from preloading, indicating that the low-temperature freezing–thawing condition would promote the porosity and have an obvious increase in damage. A continuum damage model considering subzero-temperature freezing–thawing damage from different pore sizes was finally introduced to describe the damage evolution mechanism of sandstone. The research results can be used to quantitatively evaluate the damage evolution mechanism of sandstone treated by subzero-temperature freezing–thawing without mechanical tests. Furthermore, the analysis and research results show that the damage variables of sandstone obtained by the NMR theory were lower than those of classical rock mechanics theory.
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基于核磁共振技术的预加载砂岩冻融作用损伤机理及演化模型研究
考虑到岩石内部的初始损伤,研究冻融过程中岩石的损伤退化更符合实际工程环境。本研究基于核磁共振(NMR)技术,研究了预加载和零下温度冻融的初始损伤对砂岩微观和宏观力学性能的影响。结果表明,随着初始损伤程度的增加,样品的 P 波速度降低,而孔隙率增加。对于不同预加载初始损伤程度的样品,经低温冻融-饱和处理后的 T2 信号强度分布比常温条件下的信号强度分布要大,表明低温冻融条件会促进孔隙率的增加,并有明显的损伤加剧。最后引入了考虑不同孔隙大小的亚零度冻融损伤的连续损伤模型来描述砂岩的损伤演化机制。研究结果可用于定量评估未经力学试验的亚零度冻融处理砂岩的损伤演变机制。此外,分析和研究结果表明,核磁共振理论得到的砂岩损伤变量低于经典岩石力学理论。
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来源期刊
Reviews on Advanced Materials Science
Reviews on Advanced Materials Science 工程技术-材料科学:综合
CiteScore
5.10
自引率
11.10%
发文量
43
审稿时长
3.5 months
期刊介绍: Reviews on Advanced Materials Science is a fully peer-reviewed, open access, electronic journal that publishes significant, original and relevant works in the area of theoretical and experimental studies of advanced materials. The journal provides the readers with free, instant, and permanent access to all content worldwide; and the authors with extensive promotion of published articles, long-time preservation, language-correction services, no space constraints and immediate publication. Reviews on Advanced Materials Science is listed inter alia by Clarivate Analytics (formerly Thomson Reuters) - Current Contents/Physical, Chemical, and Earth Sciences (CC/PC&ES), JCR and SCIE. Our standard policy requires each paper to be reviewed by at least two Referees and the peer-review process is single-blind.
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