日本地球惑星科学連合2023年大会

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[E] 口頭発表

セッション記号 H (地球人間圏科学) » H-DS 防災地球科学

[H-DS05] 地すべりおよび関連現象

2023年5月26日(金) 13:45 〜 15:00 106 (幕張メッセ国際会議場)

コンビーナ:王 功輝(京都大学防災研究所)、今泉 文寿(静岡大学農学部)、齋藤 仁(名古屋大学 大学院環境学研究科)、千木良 雅弘(公益財団法人 深田地質研究所)、Chairperson:William Schulz(United States Geological Survey)

14:45 〜 15:00

[HDS05-15] Decades-long landform evolution and impact of the large-scale Silabaku landslide: A case study of Yusui stream in Taiwan

*Chun-Yuan Liu1、Ching-Fang Lee1、Wei-Kai Huang1、Che-Ming Yang2、Chuan-Yi Huang1、GeoPORT working group (1.Sinotech Engineering Consultants Inc., Taiwan、2.Department of civil and disaster prevention engineering, National United University, Miaoli, Taiwan)

キーワード:Silabaku landslide, Deep-Seated Gravitational Slope Deformation, Rainfall-induced landslide, Landslide dam, Debris flow

On August 7, 2021, a devastating debris flow hit the Yusui stream in Taiwan, damaging the Minbaklu Bridge on the southern cross-island highway. The enormous quantity of debris flow was caused by a catastrophic rainfall-induced landslide at Mt. Silabaku, the source of the Yusui stream.
The main scarp of Silabaku landslide had been present for over 20 years, as identified in the historic satellite photo. The slope remained stable until typhoon Morakot struck southern Taiwan in 2009, resulting in 2486 mm of rainfall in 5 days. Over the following decade, several rainfall events further deteriorated the slope. The slope partially collapsed due to headward erosion along gullies, accompanied by spreading of the main scar and significant downward slipping of the residual slope.
This study integrates multi-temporal optical images to investigate the evolution of the Silabaku landslide and DTM data to calculate its volume. The pre-disaster LiDAR DEM reveals the deep-seated gravitational slope deformation (DSGSD) characteristics covering the entire slope surface. The slope experienced considerable displacement despite no erosion event being seen in the optical images.
After the large-scale Silabaku landslide, the DTM anomaly indicated a 60-meter subsidence in the source area and an estimated landslide volume over ten million cubic meters. The post-disaster UAV photos show evidence of a remaining landslide dam. The existence of the dam confirms that the Yusui stream was blocked, allowing water to accumulate and eventually bursting and destroying the Minbaklu Bridge in downstream.