緩勾配斜面における表層崩壊・土石流発生に及ぼす地表流の影響

Influence of Overland Flow on Occurrence of Slope Failures and Debris Flows in Gentle Slopes

秦 雅之

海堀 正博

広島大学大学院人間社会科学研究科紀要. 総合科学研究

Bulletin of the Graduate School of Humanities and Social Sciences, Hiroshima University. Studies in integrated arts and sciences

[PISSN] 2436-2603

[NCID] AA12912965

In recent years, terrible sediment disasters due to unprecedented heavy rainfalls occur frequently in Japan. One of the characteristics of these disasters is that many shallow failures occur in gentle slopes near mountain ridges where few shallow failures occurred previously. Our field survey showed a possibility that overland flow due to these unprecedented heavy rainfalls caused these slope failures. However, previous numerical models can be applied to a situation where only subsurface flow is generated, but they cannot analyze shallow failures in gentle slope areas. Therefore, we propose a method to evaluate the destabilization of the surface layer (e.g., slope failures and debris flows) caused by overland flow, assuming that the length of the slope is infinite. This method enables us to evaluate the destabilization of the surface layer in gentle slopes where the gradient is less than 20°.

slope failure

debris flow

overland flow

gentle slope

stability analysis

日本語

広島大学大学院人間社会科学研究科

掲載された論文，研究ノート，要旨などの出版権・著作権は広島大学大学院人間社会科学研究科に帰属する。 ©2020 Graduate School of Humanities and Social Sciences, Hiroshima University. All rights reserved.

[ISSN] 2436-2603

[NCID] AA12912965