CAJ | 학술논문

利用人工降雨模拟器模拟了不同历时、不同强度的降雨，对坡积层滑坡体内部的孔隙水压力、土体含水量、地下水位和斜坡表层的地表径流进行长时间序列监测，分析了近饱和坡积层斜坡入渗与地表径流的规律，揭示了监测指标对土体的变形和破坏可能的影响机制。
이용인공강우모의기모의료불동력시、불동강도적강우，대파적층활파체내부적공극수압력、토체함수량、지하수위화사파표층적지표경류진행장시간서렬감측，분석료근포화파적층사파입삼여지표경류적규률，게시료감측지표대토체적변형화파배가능적영향궤제。
The artificial rainfall simulator was used to simulate different durations, different rainfall intensities on a colluvial landslide. During the experiment period, the internal pore water pressure, soil moisture, ground-water level and surface runoff were monitored. A time series analysis was conducted based on the monitoring index on the nearly saturated colluvial slope to obtain the infiltration and runoff patterns, and to reveal the influence mechanism of monitoring indicators that affect the deformation and slope failure.