Impact of Isothermal Layering on the Stability of Saline Soil Subgrade in Cold Regions

被引:2
作者
Zhang, Yu [1 ]
Chen, Xuerui [2 ]
Zou, Meisi [3 ]
Tian, Runze [1 ]
Hou, Yunlong [4 ]
Han, Bingbing [4 ]
机构
[1] Lanzhou Jiaotong Univ, Sch Traff & Transportat, Lanzhou 730070, Peoples R China
[2] Lanzhou Rail Transit Construct Management Off, Lanzhou 730070, Peoples R China
[3] Jiujiang Vocat & Tech Coll, Sch Automot Engn, Jiujiang 332000, Jiangxi, Peoples R China
[4] Gansu Inst Engn Geol, Lanzhou 730000, Peoples R China
基金
中国国家自然科学基金;
关键词
STRENGTH;
D O I
10.1155/2022/3141964
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In order to determine the influence of heat on the stability of the saline soil subgrade slope in cold regions. Firstly, four typical representative saline soils were selected as subgrade fillers, and geotextiles were added at the bottom of the subgrade as a study subject. A two-dimensional numerical model for the temperature field of subgrade soil was established based on COMSOL Multiphysics. Secondly, combined with the main strength parameters of subgrade soil at different temperatures, an isothermal stratification-strength parameter function calculation model was proposed. Then, the SLOPE/W module in GeoStudio is used to stratify the established subgrade model according to isotherms and calculate the stability safety factor of saline soil subgrades in cold regions under different months, slopes, and subgrade heights, respectively. Finally, the influence of submergence at the foot of the slope on the stability of the subgrade slope is discussed. The results show: After the cold season coming, with the decreasing of temperature, the stability of HC-1 and HC-2 saline soil subgrade slope increased to different extents when the ground temperature dropped to -10 degrees C. When the local temperature dropped below -10 degrees C, the stability has slight decline; CS-1 and CS-2 saline soil subgrade in the ground temperature dropped to 10 degrees C (HC-1 and HC-2 denote two groups of saline soil with high chloride-salt content (>= 15%) and low sulfate salt content (<= 0.5%), whereas CS-1 and CS-2 denote two groups of saline soil with low chloride-salt (<= 5%)), the slope stability was significantly improved, and the stability of CS-1 increases slightly with further decrease in temperature.
引用
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页数:13
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