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热带海岛水工边坡风化过渡带稳定性监测试验

Stability monitoring test of weathering transition zone of hydraulic slopes in tropical island

  • 摘要: 针对气旋降雨环境下水工边坡破坏的监测理论与技术问题,开展了气旋降雨环境岩质边坡风化过渡带稳定性监测物理模型试验。结果表明:气旋降雨环境下水−气作用造成坡面侵蚀,强−弱风化过渡带的地下水压力波动是导致边坡显著变形的主要原因;降雨入渗时期边坡风化过渡带的孔隙水压力和降雨强度呈正相关,同时强−弱风化过渡带锚杆轴力损失加剧;地下水压力波动时期边坡锚固系统智能端部结构产生卸荷响应;基于锚杆轴力和孔隙水压力间的非线性关系提出了边坡风化过渡带稳定性监测判据。

     

    Abstract: In the report, aimed at the problems about the monitoring theory and technology of the hydraulic slopes failure under cyclone rainfall, a physical model test on the stability monitoring of weathering transition zone in hydraulic slopes was carried out. The results indicated that the surface erosion was caused by water-air interaction under cyclone rainfall, and the groundwater pressure fluctuation in the strong-weak weathering transition zone was the main cause of slope deformation. The pore water pressure of the slope weathering transition zone was positively correlated with rainfall intensity during rainfall infiltration, while the axial force loss of rock bolts in the weathering transition zone was intensified. The unloading response of the Intelligent Terminal Structure of the slope anchoring system was significant during the period of groundwater pressure fluctuation. Moreover, based on the nonlinear relationship between the axial force of the rock bolt and the pore water pressure, the stability monitoring criterion of weathered transition zone was proposed.

     

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