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水对红泥岩剪切行为及微观结构影响的研究

Study on the effect of water on the shear behavior and microstructure of red mudstone.

作者信息

Xie Qingyu, Huang Qiangbing, Kang Xiaosen, Wu Shaoyan, Lan Hengxing

机构信息

Department of Geological Engineering, Chang'an University, Xi'an, 710054, China.

Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an, 710054, China.

出版信息

Sci Rep. 2024 Dec 2;14(1):29858. doi: 10.1038/s41598-024-78710-x.

Abstract

Red mudstone has significant hydrophilicity, that is hard at low water contents and soft and unstable at high water contents, and understanding the whole range of water content on the shear behavior of red mudstone is critical for evaluating red beds landslide stability. However, the deterioration mechanism of red mudstone in the process of gradual humidification is not clear in the whole range of water content. In this study, a series of mechanical and microscopic tests were carried out in the whole range of water content. A mechanical behavior prediction model for the entire process under the coupling of initial damage and load damage was constructed. The results show that the deterioration of shear strength, elastic modulus and strength parameters conforms to the "logistic model" curve with the increase of water content in the whole range of water content. In addition, the water sensitivity of cohesion was higher than the internal friction angle, and it gradually stabilized as water content increased. The weakening mechanism of the mechanical strength in the accelerated decline stage is the initiation and propagation of microcracks caused by mineral expansion, which leads to the corresponding shear behavior. Finally, the constructed damage model can be transformed into different yield conditions through parameter changes. The introduction of coupling damage enables the model to more accurately describe and predict the accelerated attenuation stage of red mudstone in the process of gradual humidification in the whole range of water content.

摘要

红泥岩具有显著的亲水性,即含水量较低时坚硬,含水量较高时软且不稳定,了解含水量全范围对红泥岩剪切行为的影响对于评估红层滑坡稳定性至关重要。然而,在含水量全范围内,红泥岩在逐渐湿润过程中的劣化机制尚不清楚。本研究在含水量全范围内开展了一系列力学和微观试验。构建了初始损伤与荷载损伤耦合作用下全过程的力学行为预测模型。结果表明,在含水量全范围内,随着含水量增加,抗剪强度、弹性模量及强度参数的劣化符合“逻辑斯蒂模型”曲线。此外,黏聚力的水敏感性高于内摩擦角,且随含水量增加逐渐趋于稳定。加速下降阶段力学强度的弱化机制是矿物膨胀导致微裂纹萌生与扩展,进而引发相应的剪切行为。最后,所构建的损伤模型可通过参数变化转化为不同的屈服条件。耦合损伤的引入使模型能够更准确地描述和预测红泥岩在含水量全范围内逐渐湿润过程中的加速衰减阶段。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9200/11612310/5e8e652466fe/41598_2024_78710_Fig1_HTML.jpg

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