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Applications of SEM and ESEM in Microstructural Investigation of Shale-Weathered Expansive Soils along Swelling-Shrinkage Cycles

机译:SEM和ESEM在页岩风化膨胀土沿胀缩循环的微观结构研究中的应用

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摘要

Understanding the microstructure of expansive soils is of vital importance in physical interpretation and mechanical modeling of expansive soil behavior at the macro scale. To approach this objective, two natural expansive soils were compacted and imaged to disclose their microstructure using both conventional scanning electron microscopy (SEM) and environmental scanning electron microscopy (ESEM). The micrographs of the samples at their initial compacted state showed comparable results when using SEM and ESEM techniques. The structural changes in response to two wetting-drying cycles were monitored through the ESEM experiments in order to simulate the volumetric evolution at the macro scale. Despite the significant macroscopic volume changes, it was difficult to detect structural changes at the micro scale. The ESEM test results only qualitatively described structural shrinkage upon the first drying cycle but showed little structural modification thereafter, due to the limited duration of vapor exchange between the chamber atmosphere and the sample under the microscope. In addition, the combined effects of plasticity and original microstructure determined how the microstructure evolved as a function of sample consolidation. Based on the analysis of results, limitations of both SEM and ESEM approaches in microstructural investigations of expansive soils are discussed and summarized. (C) 2014 Elsevier B.V. All rights reserved.
机译:理解膨胀土的微观结构对于宏观解释膨胀土行为的物理解释和力学建模至关重要。为了达到这个目的,使用常规扫描电子显微镜(SEM)和环境扫描电子显微镜(ESEM)对两种天然膨胀土进行压实和成像,以揭示其微观结构。当使用SEM和ESEM技术时,样品在初始压紧状态下的显微照片显示出可比的结果。通过ESEM实验监测了响应于两个干湿循环的结构变化,以模拟宏观尺度上的体积演变。尽管宏观的体积发生了显着变化,但很难在微观尺度上检测出结构变化。 ESEM测试结果仅定性描述了第一个干燥循环后的结构收缩率,但此后由于在腔室气氛和显微镜下样品之间的蒸汽交换持续时间有限,因此几乎没有结构修饰。此外,可塑性和原始微观结构的综合作用决定了微观结构如何随着样品固结的发展而变化。在分析结果的基础上,讨论并总结了SEM和ESEM方法在膨胀土微观结构研究中的局限性。 (C)2014 Elsevier B.V.保留所有权利。

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