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Landslide model test to investigate the spreading range of debris according to rainfall intensity

机译:根据降雨强度进行滑坡模型试验以研究碎片的分布范围

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摘要

Landslide model experiments by considering rainfall intensity were performed to investigate andpredict the spreading range of debris. The model flume and the rainfall simulator were designed and manufacturedfirstly,and a series of model experiments were performed. The model experiments were performed with changingthe rainfall intensity from 150 mm/hr to 250 ram/hr. In these experiments,the angle of slope inclination is 25~ andthe relative density of slope soils is 35%. In order to measure the pore water pressure in a slope,the deformationof slope surface,and the spreading range of debris during experiments,the instrumentation was installed in theslope. As a result of instrumentation,the pore water pressure is increased rapidly at the time of landslides,andthe pore water pressure in a slope and the scale of landslide are increased with increasing the rainfall intensity.In addition,the shape of spreading range of debris looks like a bulged pan,and the spreading range is increasedrapidly in its early stage and then increased gradually. The increasing velocity of spreading range is influencedby the rainfall intensity,and the final spreading area after heavy rainfall depends on the rainfall intensity andthe rainfall duration time.
机译:结合降雨强度进行滑坡模型试验,以研究和预测泥石的传播范围。首先设计并制造了模型水槽和降雨模拟器,并进行了一系列的模型实验。通过将降雨强度从150 mm / hr更改为250 ram / hr进行模型实验。在这些实验中,斜坡的倾斜角度为25°,斜坡土壤的相对密度为35%。为了测量边坡中的孔隙水压力,边坡的变形以及在试验过程中碎屑的散布范围,将仪器安装在边坡上。仪器化的结果是,滑坡发生时孔隙水压力迅速升高,边坡的孔隙水压力和滑坡规模随着降雨强度的增加而增大。像鼓鼓的锅,其传播范围在早期迅速增加,然后逐渐增加。降雨强度影响扩散范围的增加速度,暴雨后的最终扩散面积取决于降雨强度和降雨持续时间。

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  • 来源
  • 会议地点 Xian(CN)
  • 作者单位

    Y.S. Song@Korea Institute of Geoscience Mineral Resources (KIGAM),Daejeon,Korea--B.G. Chae@Korea Institute of Geoscience Mineral Resources (KIGAM),Daejeon,Korea--Y.C. Cho@Korea Institute of Geoscience Mineral Resources (KIGAM),Daejeon,Korea--Y.S.Seo@Chung-Buk National University,Chungju,Korea--;

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  • 正文语种 eng
  • 中图分类 基础加固;
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