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杨旭, 蔡国庆, 刘倩倩, 李风增, 单冶鹏. 干湿循环对黏土微观结构及持水性能影响的试验研究[J]. 岩土工程学报, 2024, 46(S2): 11-15. DOI: 10.11779/CJGE2024S20006
引用本文: 杨旭, 蔡国庆, 刘倩倩, 李风增, 单冶鹏. 干湿循环对黏土微观结构及持水性能影响的试验研究[J]. 岩土工程学报, 2024, 46(S2): 11-15. DOI: 10.11779/CJGE2024S20006
YANG Xu, CAI Guoqing, LIU Qianqian, LI Fengzeng, SHAN Yepeng. Experimental study on influences of wetting-drying cycles on microstructure and water-retention characteristics of clay[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(S2): 11-15. DOI: 10.11779/CJGE2024S20006
Citation: YANG Xu, CAI Guoqing, LIU Qianqian, LI Fengzeng, SHAN Yepeng. Experimental study on influences of wetting-drying cycles on microstructure and water-retention characteristics of clay[J]. Chinese Journal of Geotechnical Engineering, 2024, 46(S2): 11-15. DOI: 10.11779/CJGE2024S20006

干湿循环对黏土微观结构及持水性能影响的试验研究

Experimental study on influences of wetting-drying cycles on microstructure and water-retention characteristics of clay

  • 摘要: 长期干湿循环作用会削弱路基土的工程力学性质,产生工程灾害,有必要研究干湿循环对其微观结构及持水性能的影响。针对既有线有砟轨道路基土,开展了一系列考虑干湿循环影响的压汞试验、扫描电镜试验、压力板试验与饱和盐溶液蒸汽平衡试验。试验结果表明:在反复的干湿循环过程中,土体结构遭到破坏,内部胶结物质不断减少。土体微孔及小孔(< 5 μm)数量逐渐增多,中孔及部分大孔范围(5~30 μm)内的峰值孔径逐渐减小,分布密度逐渐增大。数次干湿循环后微裂隙(> 100 μm)逐渐增多,导致试样开裂。干湿循环会对土体的持水性能产生影响,初始干密度较小时,经历过1次干湿循环持水性能略有增强,而经历过3次及5次干湿循环持水性能持续减弱。

     

    Abstract: The Long-term wetting-drying cycles can weaken the engineering characteristics of subgrade fillers, resulting in engineering disasters. It is necessary to study the effects of the wetting-drying cycles on their microstructure and water-retention performance. A series of mercury intrusion tests, scanning electron microscopy tests, pressure plate tests and saturated salt solution vapor equilibrium tests considering the influences of the wetting-drying cycles are carried out on the subgrade filler of the existing ballasted track roads. The experimental results show that during repeated wetting-drying cycles, the soil structure is damaged, and the internal cementitious materials are continuously reduced. The number of micropores and small pores (< 5 μm) in the soil gradually increases, while the peak pore size in the range of mesopores and some large pores (5~30 μm) gradually decreases, and the distribution density gradually increases. After several wetting-drying cycles, the number of microcracks (> 100 μm) gradually increases, leading to cracking of the soil specimens. The wetting-drying cycles have effects on the water-retention characteristics of the soil. When the initial dry density is low, the air-entry value after experiencing one wetting-drying cycle is slightly higher than that without wetting-drying cycles, while the air-entry value of the specimen after three and five wetting-drying cycles continues to decrease.

     

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