Investigation of tensile strength and deformation behaviors of basalt fiber-reinforced loess subjected to dry-wet cycles

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL
Zhipeng Wu, Jian Xu, Henghui Fan, Liang Li, Guochen Wang, Songhe Wang
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Abstract

The frequent occurrence of geological disasters in the Loess Plateau is related to the low tensile strength of the loess. Previous studies on fiber-reinforced loess mainly focused on compressive properties, and there have been fewer studies on tensile behaviors, especially when subjected to dry-wet cycles. In this paper, the tensile strength and deformation behaviors of basalt fiber-reinforced loess in the range of 0 to 10 dry-wet cycles were studied by uniaxial tensile test combining digital image correlation (DIC) technology. The results reveal that the unreinforced loess has no visible post-peak curve and brittle fracture occurs, while the reinforced loess has a residual strength and shows distinct ductile failure. The uniaxial tensile strength (UTS) of reinforced loess decreases with dry-wet cycles, but the decay rate decreases. The resistance of reinforced loess to dry-wet action is better than loess, with an optimal fiber content of 0.6%. The variation of failure strain of reinforced loess is consistent with UTS with a linear correlation between the two, indicating that the strength is directly related to its deformation resistance. The maximum axial strain in the surface strain field of reinforced loess shows an increasing trend with dry-wet cycles and a decreasing and then increasing trend with fiber content, which is opposite to UTS and failure strain. Fiber reinforcement improves the plastic properties of loess, and the deformation of reinforced loess is more uniform. This study reveals the deterioration law of reinforced loess under dry-wet cycles, providing theoretical support for engineering construction in loess areas.

Abstract Image

干湿循环作用下玄武岩纤维增强黄土抗拉强度及变形特性研究
黄土高原地质灾害频发与黄土抗拉强度低有关。以往对纤维增强黄土的研究主要集中在压缩特性上,而对其拉伸特性,特别是干湿循环下的拉伸特性研究较少。本文采用单轴拉伸试验结合数字图像相关(DIC)技术,研究了玄武岩纤维增强黄土在0 ~ 10个干湿循环范围内的抗拉强度和变形特性。结果表明:未加筋黄土无明显峰后曲线,出现脆性断裂;加筋黄土有残余强度,表现出明显的延性破坏;加筋黄土的单轴抗拉强度随干湿循环而减小,但衰减率减小。加筋黄土的抗干湿作用性能优于黄土,纤维含量为0.6%为最佳。加筋黄土的破坏应变变化与UTS一致,两者呈线性相关关系,说明强度与其抗变形能力直接相关。加筋黄土表面应变场最大轴向应变随干湿循环增加呈增大趋势,随纤维含量增加呈先减小后增大趋势,与UTS和破坏应变相反。纤维增强改善了黄土的塑性性能,增强后的黄土变形更加均匀。揭示了干湿循环作用下加筋黄土的劣化规律,为黄土地区的工程建设提供理论支持。
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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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