• Search Research Projects
  • Search Researchers
  • How to Use
  1. Back to project page

2023 Fiscal Year Final Research Report

Evaluation of regional peculiarities focusing on external forces and boundary conditions that cause widespread shallow landslides

Research Project

  • PDF
Project/Area Number 21H01581
Research Category

Grant-in-Aid for Scientific Research (B)

Allocation TypeSingle-year Grants
Section一般
Review Section Basic Section 25030:Disaster prevention engineering-related
Research InstitutionHokkaido University

Principal Investigator

Koi Takashi  北海道大学, 広域複合災害研究センター, 准教授 (40845294)

Co-Investigator(Kenkyū-buntansha) 堀田 紀文  東京大学, 大学院農学生命科学研究科(農学部), 准教授 (00323478)
吉本 充宏  山梨県富士山科学研究所, その他部局等, 研究員 (20334287)
執印 康裕  九州大学, 農学研究院, 教授 (60221305)
Project Period (FY) 2021-04-01 – 2024-03-31
Keywords地震 / 表層崩壊 / 緩勾配斜面 / 外力 / 境界条件 / 地震動 / ハザードエリア / 大規模表層崩壊
Outline of Final Research Achievements

Through field surveys and existing reports, the slip surface was identified, and the depth of the slip surface was estimated by correlating isopacks organized by eruption data. Additionally, slope stability analysis was conducted, utilizing physical properties of volcanic ejecta samples collected at the site as parameters, leading to a clear understanding of landslide occurrence conditions. The results indicate that the volcanic ejecta, acting as the slip surface, has retained its sedimentary structure from the time of eruption, spanning several thousand years, and was susceptible to failure due to the combination of gentle slope angles and strong seismic vibrations. By comprehending the underlying mechanisms of these earthquake-induced landslides, we can enhance preparedness and response strategies in volcanic regions prone to seismic activity, reducing the potential impact of future events.

Free Research Field

砂防学

Academic Significance and Societal Importance of the Research Achievements

地震に伴う強振動により斜面崩壊が発生した場合,避難のリードタイムがほとんどなく,甚大な被害を引き起こすことがある。特に,2018年北海道胆振東部地震では,勾配が20度から30度の斜面で最も多くの崩壊が発生し大きな人的被害が生じた。わが国ではこうした緩勾配斜面は,法律上も防災対策の検討対象となっていない。したがって,本研究課題で取り扱った大規模表層崩壊の地形的・地質的特徴を把握し,その発生機構を明らかにしたことは学術的に重要な知見であり,また,これまで想定されていなかったハザードエリアを潜在的に示すことができたことで,山地防災に係る対策を検討することが可能となったことは社会的意義が大きい。

URL: 

Published: 2025-01-30  

Information User Guide FAQ News Terms of Use Attribution of KAKENHI

Powered by NII kakenhi