Xi'n University of Science and Technology, Xi'an, 710054, China.
Qinghai Bureau of Coal Geology, Xining, 810012, China.
Sci Rep. 2020 Dec 9;10(1):21569. doi: 10.1038/s41598-020-78489-7.
Soil-Water characteristic Curve (SWCC) is meant to describe the mechanical behavior of unsaturated soil. The present paper focuses on the internal multi-scale microstructure of Xining untreated loess and lime-treated loess with the use of scanning electron microscopy (SEM) and image processing technique. A new SWCC model was presented based on the fractal dimension of pore size distribution. The SWCC of untreated loess was calculated from fractal dimension and fitted well with curve tested from Fredlund SWCC device. The SWCC of lime-treated loess was then calculated. Two curves of Xining untreated loess and lime-treated loess have been compared and reasons for the difference have also been discussed. The results indicate that the content of large pores in lime-treated loess decreased and the content of micro-pore increased. The bracket pores were changed into cement pores. The pore fractal dimension D of Xining untreated loess is 1.39 and the pore fractal dimension D of Xining lime-treated loess is 1.53. Air-entry value of untreated loess is 12.16 kPa, while lime-treated Loess-35.15 kPa. In transition region, matric suction of lime-treated loess was in the range of 35.15 kPa ~ 4000 kPa, while matric suction of untreated loess-12.16 kPa ~ 2600 kPa. The range of the transition region in lime-treated loess is larger than that in the loess, while in the range of saturation region, the reverse applies. Under the condition of the same matrix suction, the saturation of lime-treated loess is greater than that of untreated loess. In the residual region, the difference of SWCC of soil samples is small.
土壤-水特征曲线(SWCC)用于描述非饱和土的力学行为。本文利用扫描电子显微镜(SEM)和图像处理技术,重点研究了西宁原状黄土和石灰处理黄土的内部多尺度微观结构。提出了一种基于孔径分布分形维数的新的 SWCC 模型。利用分形维数计算了原状黄土的 SWCC,并与弗雷德隆德 SWCC 装置测试的曲线拟合良好。然后计算了石灰处理黄土的 SWCC。比较了西宁原状黄土和石灰处理黄土的 SWCC,并讨论了差异的原因。结果表明,石灰处理黄土中大孔含量减少,微孔含量增加。支架孔变成水泥孔。西宁原状黄土的孔隙分形维数 D 为 1.39,西宁石灰处理黄土的孔隙分形维数 D 为 1.53。原状黄土的进气值为 12.16 kPa,而石灰处理黄土为 35.15 kPa。在过渡区,石灰处理黄土的基质吸力范围为 35.15 kPa4000 kPa,而原状黄土的基质吸力范围为 12.16 kPa2600 kPa。石灰处理黄土过渡区的范围大于原状黄土,而在饱和区范围内则相反。在相同基质吸力条件下,石灰处理黄土的饱和度大于原状黄土。在残余区,土样 SWCC 的差异较小。