国立研究開発法人土木研究所

論文・刊行物検索

利用者の方へ

詳細情報

発表 International Journal of Erosion Control Engineering Analysis for a landslide dam outburst flood in Ambon Island, Indonesia

作成年度 2015 年度
論文名 International Journal of Erosion Control Engineering Analysis for a landslide dam outburst flood in Ambon Island, Indonesia
論文名(和訳)
論文副題
発表会 6th International Conference on Debris-Flow Hazards Mitigation
誌名 6th International Conference on Debris-Flow Hazards Mitigation
巻・号・回
発表年月日 2015/06/22 ~ 2015/06/25
所属研究室/機関名 著者名(英名)
Volcano and Debris Flow Research TeamTadanori ISHIZUKA
TOKEN C.E.E. Consultants Co., Ltd.Akihito KAJI
Ministry of Land, Infrastructure, Transport and TourismKoji MORITA
Sabo Frontier FoundationToshio MORI
Sabo Frontier FoundationMiki CHIBA
抄録
In July 2012, a landslide dam subsequent to the large-scale collapse of a mountain edifice occurred on Ambon Island in the eastern part of Indonesia. A height of the dam was approximately 140 m and a volume of dammed water was approximately 250 million m3. The dam failed about a year after its formation in July 2013, and a large-scale flood wreaked havoc on the downstream area. In this disaster, the information on the topographic changes before and after the dam failure was obtained from digital maps (DEM) based on satellite images and field measurement. Furthermore, field surveys examined the various conditions of the sites around the landslide dam and a process of the outburst flood was recorded on video. Simulation of a landslide dam outburst flood was conducted using LADOF model that reproduces the process of overflow and erosion of a landslide dam outbreak and the calculation result was verified by field measurement data. The results are as follows. (1)The peak flow rate of the landslide dam outburst flood determined by simulation was approximately 17,000 m3/s. (2)The occurrence and duration of the flood, longitudinal profile of the dam, inundated area and flow depth obtained from the simulation almost agree with the actual results obtained from field measurement. (3)The phenomena whereby the progress of longitudinal erosion caused the collapse of the stream bank and rapidly expanded the river channel width could be confirmed by analysis of the video images.
ページの先頭へ

この画面を閉じる

Copyright (C) 2022 Independent Administrative Institution Public Works Research Institute