日本地球惑星科学連合2024年大会

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[E] ポスター発表

セッション記号 H (地球人間圏科学) » H-DS 防災地球科学

[H-DS08] 地すべりおよび関連現象

2024年5月31日(金) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:王 功輝(京都大学防災研究所)、千木良 雅弘(公益財団法人 深田地質研究所)、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)

17:15 〜 18:45

[HDS08-P02] Landslide Susceptibility Analysis and Mapping in Northern Kyushu Area Using Slope Hazard History and Geological Information

*川畑 大作1宮地 良典1阿部 朋弥1斎藤 眞1、井柳 卓也2、小林 央宜2、大石 博之2内村 公大2水落 裕樹1宮川 歩夢1 (1.国立研究開発法人 産業技術総合研究所、2.西日本技術開発株式会社)

キーワード:地すべり、すべりやすさマップ、シームレス地質図

The basic factors for landslide occurrence are influenced by multiple conditions such as topography, geology, and vegetation. Spatial information on these factors and past landslide histories can be used to determine which conditions predispose to the occurrence of landslides. In this study, an inventory dataset of topography, geology, and disaster history was compiled mainly for the northern Kyushu region, where heavy rainfall disasters have occurred frequently in recent years. Using 10-m mesh data from the Fundamental Geospatial Data (FGD) by GSI, we developed a topographic inventory of topographic features such as slope and relative relief, and a topographic inventory of watersheds. For the geologic inventory, we used Seamless digital geological map of Japan V2 1:200,000 and classified the geologic divisions into age data and lithologic facies. The same geological features that have been contact metamorphosed by igneous intrusions are harder and less susceptible to collapse. Therefore, the distribution of contact metamorphic zones should be classified in terms of landslide susceptibility and landslide occurrence among geological features of the same type. As data on past landslides to compare with these predispositions, we collected digital archive for landslide distribution map by the National Research Institute for Earth Science and Disaster Resilience (NIED) and information maintained by local governments and organizations and created an inventory data of landslide history.
In this study, using the inventory data, we analyzed the relationship between past landslides and their predisposing factors by dividing them into three categories: rainfall-induced, earthquake-induced, and other factors. In recent years, many studies have also used machine learning and other techniques for hazard mapping. Landslide susceptibility was mapped using multiple methods in this study.