非饱和红砂岩风化土土水特征及降雨对其边坡稳定性的影响

Soil and water characteristics of unsaturated red sandstone weathered soil and effects of rainfall on its slope stability

  • 摘要: 为防止非饱和红砂岩风化土边坡因水分状态的变化出现失稳破坏,对其开展土水特征及降雨作用下稳定性变化研究。首先,针对不同初始干密度、初始质量含水率条件下的非饱和红砂岩风化土进行脱湿试验,得到其土水特征曲线,通过分析其规律,提出改进指数函数模型,并与F-X模型进行对比。应用该模型进行数值模拟,分析降雨强度及时长对边坡稳定性的影响。结果表明:在参数更少、表达形式更简洁的条件下,改进的指数函数模型达到了与F-X模型相近的拟合精度,并且对残余含水率的估算结果更准确,对红砂岩风化土具有更好的适用性;在降雨持时相同时,降雨强度增大,坡体饱和度增加,边坡稳定性降低;随着降水持时延长,0~6 h段边坡稳定性显著降低,之后稳定性下降较小;短时间的强降雨对于红砂岩风化土边坡稳定性影响较大。

     

    Abstract: In order to prevent the unstable damage of unsaturated red sandstone weathered soil slopes due to the changes in water state, a study of soil and water characteristics and stability changes under the action of rainfall was carried out. First, the dehumidifying test was conducted on the unsaturated red sandstone weathered soil under different initial dry densities and initial mass moisture contents, with soil and water characteristic curve obtained. By analyzing its rules, an improved exponential function model was proposed and compared with the F-X model. Finally, the model was applied to carry out numerical simulation, analyzing the effects of rainfall intensity and duration on slope stability. The results show that under the condition of fewer parameters and more concise expression, the improved exponential function model achieves a fitting accuracy close to that of the F-X model, and the estimation result of residual water content is more accurate, with better applicability to red sandstone weathered soil. When the rainfall holding time is the same, the rainfall intensity and slope saturation increases, but slope stability decreases. With the extension of precipitation, the slope stability is significantly reduced in 0‒6 h, and after that the stability is less reduced. The short period of heavy rainfall has a great influence on the stability of red sandstone weathered soil slope.

     

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