Influence of dry density and wetting-drying cycles on the soil-water retention curve of compacted loess: experimental data and modeling

被引:7
|
作者
Yuan, Kangze [1 ,2 ,3 ]
Ni, Wankui [2 ]
Della Vecchia, Gabriele [3 ]
Lu, Xiangfei [2 ]
Wang, Haiman [2 ]
Nie, Yongpeng [2 ]
机构
[1] Northwest Univ, Geol Dept, State Key Lab Continental Dynam, Xian 710069, Peoples R China
[2] Changan Univ, Coll Geol Engn & Geomat, 126 Yanta Rd, Xian 710054, Shaanxi, Peoples R China
[3] Politecn Milan, Dept Civil & Environm Engn, Piazza Leonardo Vinci 32, I-20133 Milan, Italy
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
Compacted loess; Dry density; Soil-water retention curve; Wetting-drying cycles; PORE-SIZE DISTRIBUTION; MERCURY INTRUSION; SHEAR-STRENGTH; MICROSTRUCTURAL EVOLUTION; MECHANICAL-PROPERTIES; CLAY; BEHAVIOR; PLATEAU; DISTRIBUTIONS; COLLAPSIBILITY;
D O I
10.1007/s11440-024-02354-4
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In this paper, the EC-5 water sensor and the MPS-6 water potential sensor were used to measure water content and suction, respectively, to investigate the evolution of soil-water retention properties of compacted loess samples prepared at different dry densities and subjected to different numbers of wetting-drying cycles. The water retention data were integrated with a detailed microstructural investigation, including morphological analysis (by scanning electron microscopy) and pore size distribution determination (by nuclear magnetic resonance). The microstructural information obtained shed light on the double porosity nature of compacted loess, allowing the identification of the effects of compaction dry density and wetting-drying cycles at both intra- and inter-aggregate levels. The information obtained at the microstructural scale was used to provide a solid physical basis for the development of a simplified version of the water retention model presented in Della Vecchia et al. (Int J Numer Anal Meth Geomech 39: 702-723, 2015). The model, adapted for engineering application to compacted loess, requires only five parameters to capture the water retention properties of samples characterized by different compaction dry densities and subjected to different numbers of wetting-drying cycles. The comparison between numerical simulations and experimental results, both original and from the literature, shows that only one set of parameters is needed to reproduce the effects of dry density variation, while the variation of only one parameter allows the reproduction of the effects of wetting and drying cycles. With respect to the approaches presented in the literature, where ad hoc calibrations are often used to fit density and wetting-drying cycle effects, the model presented here shows a good compromise between simplicity and predictive capabilities, making it suitable for practical engineering applications.
引用
收藏
页码:8111 / 8128
页数:18
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