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Study on Seepage Laws of Completely Weathered Phyllite Slope Under Rainfall

机译:降雨条件下完全风化的玄武岩坡面渗流规律研究

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According to the available geological data and monitoring data, the completely weathered phyllite slope dilates and softens under the condition of continuous rainfall, which is then prone to instability failure. The indoor artificial rainfall test was carried out through the construction of the slope model, and the soil moisture sensor, pore water pressure sensor and matric suction sensor were used to study the variation laws of moisture content, pore water pressure and infiltration line at the back edge, slope body and the foot of the slope under continuous heavy rainfall. According to the sensor data and recorded information, with the influence of heavy rainfall over a long period of time, the water content and pore water pressure increased firstly, then decreased, and finally stabilized. The infiltration line moved from the top, the surface and the foot of the slope to the slope body, and shallow slip failure occurred in the shallow layer of the slope body.
机译:根据现有的地质资料和监测资料,完全风化的千枚岩斜坡在连续降雨的条件下会膨胀并软化,从而容易发生失稳。通过建立边坡模型进行室内人工降雨试验,并利用土壤水分传感器,孔隙水压力传感器和基质吸力传感器研究了水分,背面孔隙水压力和入渗线的变化规律。在连续大量降雨的情况下,边沿,坡体和坡脚。根据传感器数据和记录的信息,在长时间的强降雨影响下,水含量和孔隙水压力先升高,然后降低,最终稳定。入渗线从斜坡的顶部,表面和脚向斜坡体移动,在斜坡体的浅层发生了浅层滑动破坏。

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