Advanced multi-scale characterization of loess microstructure: Integrating μXCT and FIB-SEM for detailed fabric analysis and geotechnical implications

IF 6.9 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
B. Yu , T.A. Dijkstra , W. Fan , I.J. Smalley , Y.N. Wei , L.S. Deng
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Abstract

Loess, a Quaternary wind-blown deposit, is a problem soil that gives rise to frequent geohazards such as landslides and water-induced subsidence. The behaviour of loess is controlled by its microstructure, consisting of silt-sized skeleton particles and complex bonding structures formed by clay-sized particles. Achieving a deep understanding and precise modelling of loess behaviour necessitates comprehensive knowledge of the realistic 3D microstructure. In this paper, a correlative investigation of the 3D loess microstructure is performed using X-ray micro-computed tomography (μXCT) and focused ion beam scanning electron microscope (FIB-SEM). Details of clay structures in loess, such as clay coatings, clay bridges and clay buttresses, are visualized and characterized in 3D based on FIB-SEM images with a voxel size of 10 × 10 × 10 nm3. The clay structures exhibit a diverse degree of complexity and their impact on the mechanical properties of loess is highlighted. Statistical analysis of the skeleton particles, including size, shape and orientation, are derived from μXCT images with a voxel size of 0.7 × 0.7 × 0.7 μm3. The findings provide insights into the collapse mechanism and particle-scale modelling of loess. The combination of μXCT and FIB-SEM proves to be a powerful approach for characterizing the intricate micro-structures of loess, as well as other geomaterials.

黄土微观结构的先进多尺度表征:整合 μXCT 和 FIB-SEM,进行详细的结构分析和岩土工程影响分析
黄土是第四纪风吹沉积物,是一种问题土壤,经常引发滑坡和水引起的沉降等地质灾害。黄土的行为受其微观结构控制,由淤泥大小的骨架颗粒和粘土大小的颗粒形成的复杂粘结结构组成。要深入了解黄土的行为并建立精确的模型,就必须全面了解其逼真的三维微观结构。本文利用 X 射线显微计算机断层扫描(μXCT)和聚焦离子束扫描电子显微镜(FIB-SEM)对黄土的三维微观结构进行了相关研究。基于体素尺寸为 10 × 10 × 10 nm3 的 FIB-SEM 图像,对黄土中粘土结构的细节,如粘土涂层、粘土桥和粘土支撑进行了三维可视化和表征。粘土结构呈现出不同程度的复杂性,它们对黄土力学性能的影响也得到了强调。通过体素尺寸为 0.7 × 0.7 × 0.7 μm3 的 μXCT 图像得出了骨架颗粒的统计分析结果,包括尺寸、形状和取向。研究结果为黄土的崩塌机制和颗粒尺度建模提供了启示。事实证明,μXCT 和 FIB-SEM 的结合是表征黄土以及其他土工材料复杂微观结构的有力方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Engineering Geology
Engineering Geology 地学-地球科学综合
CiteScore
13.70
自引率
12.20%
发文量
327
审稿时长
5.6 months
期刊介绍: Engineering Geology, an international interdisciplinary journal, serves as a bridge between earth sciences and engineering, focusing on geological and geotechnical engineering. It welcomes studies with relevance to engineering, environmental concerns, and safety, catering to engineering geologists with backgrounds in geology or civil/mining engineering. Topics include applied geomorphology, structural geology, geophysics, geochemistry, environmental geology, hydrogeology, land use planning, natural hazards, remote sensing, soil and rock mechanics, and applied geotechnical engineering. The journal provides a platform for research at the intersection of geology and engineering disciplines.
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