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高校地质学报 ›› 2023, Vol. 29 ›› Issue (2): 280-288.DOI: 10.16108/j.issn1006-7493.2021048

• 工程地质学 • 上一篇    下一篇

浸水作用下湿陷性黄土微观结构及分形特征研究

王绅皓,谢婉丽*,常一伦,单 帅,井 旭   

  1. 西北大学 地质学系,大陆动力学国家重点实验室,西安 710069
  • 出版日期:2023-04-20 发布日期:2023-04-20

Microstructures and Fractal Characteristics of Collapsible Loess Subjected to Water Immersion

WANG Shenhao,XIE Wanli*,CHANG Yilun,SHAN Shuai,JING Xu   

  1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi′an 710069, China
  • Online:2023-04-20 Published:2023-04-20

摘要: 针对延安新区湿陷性黄土,开展浸水试验,利用扫描电子显微镜获得不同浸水时长的黄土微观结构图像。运用ImagePro Plus(IPP)图像处理软件提取黄土的微观结构参数,结合分形理论对黄土的微观结构进行定量分析。结果表明:在浸水过程中,土体宏观表现为湿陷性减弱。土体颗粒排列、形态分布呈规律性变化;孔隙面积概率分布指数和颗粒分形维数均出现减小趋势,颗粒圆形度先减小后增大,排列发生定向改变;浸水作用对黄土微观结构的影响具有时效性,初始阶段土体受黏土矿物软化、可溶盐流失的影响,天然结构在水体扰动下逐渐失稳;随浸水时间的增加,骨架结构产生破坏,颗粒发生偏转、滑移、重组;平衡阶段颗粒形成新的结构,排列密集化,大、中孔隙减少,土体结构逐渐稳定。研究从宏观、微观两个角度研究了浸水作用下的黄土结构特征,为湿陷性黄土地区的工程问题提供了试验基础和科学依据。

关键词: 黄土, 浸水作用, 微观结构, 定量分析, 湿陷性

Abstract: The collapsible loess in Yan′an New Area was chosen to carry out the immersion test and the microstructure images of loess with different immersion periods were obtained by scanning electron microscope. The image processing software Image Pro Plus (IPP) was used to extract the microstructure parameters of loess, and the microstructure of loess was quantitatively analyzed with the fractal theory. The results show that the collapsibility of soil decreases during the immersion process. The arrangement and form distribution of soil particles change regularly. Also, both the probability distribution index of pore area and the fractal dimension of particles showed a decreasing trend, the roundness of particles first decreased and then increased, and the alignment of particles changed in direction with the time of immersion. Furthermore, the influence of water immersion on the microstructures of loess is time-sensitive. In the initial stage, the soil is affected by softening of clay minerals and the loss of soluble salts, and the natural structure gradually becomes unstable under the disturbance of water; As the immersion continues, the skeleton structure is damaged, and the particles deflect, slip, and recombine; In the equilibrium stage, the particles form new structures and become
denser, the large and medium pores decrease, and the soil structure gradually stabilizes. In this paper, the characteristics of loess structures under the action of flooding are studied from both macroscopic and microscopic perspectives, which provides an experimental and scientific basis for engineering problems in collapsible loess areas.

Key words: loess, immersion action, microstructure, quantitative analysis, collapsibility

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