首页> 外文期刊>Bulletin of engineering geology and the environment >Unconfined compression behavior of basalt fiber-reinforced loess based on digital image correlation and scanning electron microscope
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Unconfined compression behavior of basalt fiber-reinforced loess based on digital image correlation and scanning electron microscope

机译:基于数字图像关联和扫描电子显微镜的玄武岩纤维增强黄土无侧压行为

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摘要

Basalt fiber is a promising reinforcement agent for loess engineering. In this study, unconfined compressive tests facilitatedwith the digital image correlation (3D-DIC) method were carried out on basalt fiber-reinforced loess to obtain the deformationimages and surface strain fields at different loading moments. The reinforcement mechanism of samples with differentfiber contents and fiber lengths was interpreted from the microstructure obtained by scanning electron microscope (SEM).Results showed that the stress-strain curves of fiber-reinforced samples are all strain-softening. The curves of unconfinedcompressive strength (UCS) versus fiber length or fiber content manifest an overall inverted U-shaped pattern. The optimalreinforcement effect was observed at a fiber content of 0.6 and a fiber length of 12 mm. The failure strain, plasticityratio, and energy absorption capacity of samples vary with fiber content or fiber length like that of the UCS. Fracture ofunreinforced loess was noted, characterized by brittle failure, while the reinforced loess exhibits bulging failure with ductilecharacteristics. The surface strain field shows that the maximum axial strain varies with fiber content and fiber length incontrast to the strength. The deformation of the sample is more uniform under the optimal fiber condition, and the effect offiber content is significantly greater than that of fiber length. SEM images indicate that the fibers are more uniformly distributedin the soil at lower fiber contents and smaller fiber lengths. Otherwise, significant entanglement or agglomerationwill occur, resulting in the creation of weak surfaces in the soil.
机译:玄武岩纤维是一种很有前途的黄土工程增强剂。本研究采用数字图像相关(3D-DIC)方法对玄武岩纤维增强黄土进行无侧限抗压试验,得到不同加载力矩下的变形图像和表面应变场。从扫描电子显微镜(SEM)获得的微观结构中解读了不同纤维含量和纤维长度样品的增强机理。结果表明:纤维增强试样的应力-应变曲线均呈应变软化趋势。无限制抗压强度 (UCS) 与纤维长度或纤维含量的曲线呈现整体倒 U 形图案。在纤维含量为0.6%且纤维长度为12 mm时,观察到最佳的增强效果。样品的失效应变、塑性比和能量吸收能力随纤维含量或纤维长度而变化,就像UCS一样。未加固黄土出现断裂,表现为脆性破坏,而加筋黄土则表现为具有韧性特征的凸起破坏。表面应变场表明,最大轴向应变随纤维含量和纤维长度的变化而变化,与强度无关。在最佳纤维条件下,试样的变形更加均匀,纤维含量的影响明显大于纤维长度的影响。SEM图像表明,纤维含量较低,纤维长度较小,纤维分布更均匀。否则,将发生严重的缠结或团聚,导致土壤中产生薄弱的表面。

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