Key influencing factors and prediction model for the tensile strength of compacted clayey loess

IF 4.2 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Lulu Liu, Tong Liu, Xiaoyan Liu, Zhe Li, Guojun Cai
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Abstract

The tensile strength of loess directly impacts the stability and safety of engineering constructions in loess regions. To systematically investigate the key factors influencing the tensile strength of compacted loess, uniaxial tensile tests were conducted on loess samples using a self-developed high-precision uniaxial testing apparatus. The effects of saturation and tensile rate were analyzed, and a mathematical model was developed to predict the tensile strength of compacted loess. Additionally, the dynamic tensile behavior of loess under stepwise loading was studied to examine the rate effect. The microstructural characteristics of clayey loess at different moisture contents were also explored to help explain the underlying mechanisms. The results showed that the relationship between saturation and tensile strength in clayey loess is asymmetric. Water’s influence on clayey loess is not only related to capillary suction but also to the hydration of the clay particles. The relationship between tensile rate and tensile strength exhibited a nonlinear enhancement: the higher the rate, the slower the increase in tensile strength. As the tensile rate increased, the stress–strain curve of the soil exhibited more brittle fracture characteristics. Under stepwise tensile conditions, the tensile rate in the second stage was negatively correlated with the ultimate tensile strain. Based on the experimental results, a reliable prediction model was established to forecast the tensile strength of compacted loess under various key influencing factors. These findings provide theoretical insights for engineering design and soil improvement technologies in loess regions.

Abstract Image

粘性土压实抗拉强度关键影响因素及预测模型
黄土的抗拉强度直接影响到黄土地区工程建设的稳定性和安全性。为系统研究影响压实黄土抗拉强度的关键因素,采用自行研制的高精度单轴试验装置对黄土试样进行了单轴抗拉试验。分析了饱和度和拉伸速率对压实黄土抗拉强度的影响,建立了压实黄土抗拉强度的数学模型。此外,还研究了黄土在逐级加载下的动态拉伸特性,以检验速率效应。探讨了不同含水率下粘性黄土的微观结构特征,有助于解释其潜在机制。结果表明,粘性黄土的饱和度与抗拉强度之间存在不对称关系。水对粘性黄土的影响不仅与毛细吸力有关,还与粘土颗粒的水化作用有关。拉伸速率与拉伸强度呈非线性增强关系:速率越高,拉伸强度增长越慢。随着拉伸速率的增加,土体的应力-应变曲线呈现出更明显的脆性断裂特征。在逐级拉伸条件下,第二阶段的拉伸速率与极限拉伸应变呈负相关。在试验结果的基础上,建立了一个可靠的预测模型,用于预测各种关键影响因素下压实黄土的抗拉强度。这些发现为黄土地区的工程设计和土壤改良技术提供了理论依据。
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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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