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Landslide and mudflow disaster in disposal site of surplus soil at Higashi-Hiroshima due to heavy rainfall in 2009

机译:2009年强降雨导致东广岛剩余土壤处置场发生滑坡和泥石流灾害

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摘要

The collapse of a filling occurred due to heavy rain in Higashi-Hiroshima City's Shiwa District at about 5:30 am July 25th, 2009. The filling was made of surplus soils, and it contained a mass of water supplied from rainfall and ground water flow of a permeable layer at the bottom of the filling. The collapsed soil flowed down and destroyed a house. In this paper, the cause of this disaster is discussed. The site of the disaster was used as the dumping site of surplus soils, after several changes of ground formation. The history of the geographical change was reconstructed by the image processing of old map, aerial photographs, result of 3-dimentional laser survey carried out after collapse and the measurement of thickness of collapsed soil by dynamic cone penetration test. According to the result of processing, the shape and the size of the filling before collapse was reconstructed. The relationship between the rainfall and the groundwater in the river sediments layer over which the filling was constructed was determined. A stability analysis of the filling was conducted considering the rise of the groundwater level in the filling and the laboratory measured strength parameters. The results of the stability analysis showed that the collapse would have taken place when the groundwater level rose by about 9 m due to the supply of groundwater through the river sediments layer.
机译:2009年7月25日上午5:30左右,东广岛市Shiwa区发生暴雨,导致填充物坍塌。填充物由多余的土壤制成,其中包含大量的降雨和地下水流。填充物底部的可渗透层的数量。坍塌的土壤流了下来并摧毁了房屋。本文讨论了这场灾难的原因。在几次地层变化之后,灾难的地点被用作剩余土壤的倾倒地点。地理变化的历史是通过对旧地图的图像处理,航拍照片,坍塌后进行的三维激光勘测结果以及通过动态圆锥穿透试验测量塌陷的土壤厚度来重建的。根据处理结果,重建倒塌前填充物的形状和大小。确定了降雨和河流沉积层中地下水的关系,在该沉积层上构造了填充物。考虑到填充物中地下水位的升高和实验室测得的强度参数,对填充物进行了稳定性分析。稳定性分析的结果表明,由于通过河流沉积层供应地下水,当地下水位上升约9 m时,就会发生塌陷。

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