基于CT实时扫描的非饱和黄土增湿湿陷损伤演化研究

    Investigation into the evolution of wetting-induced collapse damage in unsaturated loess using real-time CT scanning

    • 摘要: 水力作用下非饱和黄土结构性破坏是导致湿陷发生的重要原因之一,以往研究鲜有通过CT扫描揭示水分入渗动态过程对黄土湿陷变形与细观结构演化的时空关系。本文以非饱和Q3原状黄土及其重塑土为研究对象,利用自主研发的微型CT-三轴仪,开展控制围压(50~300 kPa)为常数的各向等压加载浸水试验,实现试样纵向大断面的实时动态CT扫描,揭示非饱和黄土在增湿过程中水分入渗-结构损伤-湿陷变形的跨尺度作用机制。研究结果表明原状黄土湿陷体应变要高于重塑黄土,同一围压下差异达到20.5%~90.4%,且围压升高使原状黄土浸水量减小8%~22%,湿陷响应时间缩短。CT图像显示原状黄土湿润锋沿大孔隙优势路径迁移,大孔隙在浸水后快速塌陷与胶结物富集区的软化,导致湿陷变形增大;重塑黄土因均质微小孔隙结构,湿润锋呈均匀扩散,湿陷响应平缓。围压通过“短期抑制-长期促进”双重路径影响湿陷行为,短期内压缩孔隙延缓水分入渗,湿陷响应滞后;长期会加剧孔隙坍塌,最终放大湿陷体应变。基于CT数定义结构性参数,提出黄土湿陷变形中的损伤演化方程,考虑了围压与饱和度增量对湿陷损伤的影响。研究结果阐明了结构性黄土湿陷的“优势渗流-胶结劣化”主导机制,为丰富和发展黄土结构性与湿陷机理研究提供有益基础。

       

      Abstract: Hydraulic-induced structural damage in unsaturated loess represents a key factor contributing to collapse. Previous studies rarely used CT scanning to reveal the spatio-temporal relationship between the collapsibility deformation and the microstructure evolution of loess through the dynamic process of water infiltration. In this paper, the undisturbed and remolded Q3 unsaturated loess are taken as the research subjects. Utilizing the self-developed micro-CT-triaxial apparatus, the isotropic pressure loading and water immersion tests with a constant confining pressure (50-300 kPa) are carried out. The real-time dynamic CT scanning of the longitudinal large sections of the specimens is achieved, revealing the cross-scale interaction mechanism of water infiltration - structural damage - collapse deformation during the wetting process of unsaturated loess. The results show that the collapse volumetric strain of undisturbed loess is higher than that of remolded loess, with a difference of 20.5% to 90.4% under the same confining pressure. Additionally, an increase in confining pressure reduces the immersion amount of undisturbed loess by 8% to 22% and shortens the response time of collapse. CT images demonstrate that the wetting front of undisturbed loess migrates along the dominant path of macropores, and the macropores collapse rapidly after flooding and soften the cement-rich area, resulting in the increase of collapsibility deformation. Due to the homogeneous micro-pore structure, the wetting front is uniformly diffused and the collapse response is gentle. Confining pressure influences the collapse behavior via a dual route of "short-term inhibition - long-term promotion": in the short term, it compresses pores to retard water infiltration and causes a delay in the collapse response; in the long term, it aggravates pore collapse and ultimately magnifies the volumetric strain of the collapse. Based on the CT number, a structural parameter is defined, and a damage evolution equation for loess collapse deformation is proposed, taking into account the effects of confining pressure and saturation increment on collapse damage. The research results clarify the dominant mechanism of "preferential seepage - cementation deterioration" in the structural collapsibility of loess, providing a beneficial foundation for enriching and developing the research on the structure and collapsibility mechanism of loess.

       

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