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Hazard Evaluation for Landslide Akiyuki Kawasaki, Doctoral Student Graduate School of Engineering, Yokohama National University, Japan
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Where is Yokohama?
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Background ・ Concentrated heavy rain strikes Japan every year ・ Many houses and buildings are damaged and lives are lost in the landslide and debris flow. ⇒ There are two major problems. ・ However, Existing policy is not enough. ⇒ Good policy is needed.
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1. Problems in Policy “Hazard zone for landslide” is specified by Municipal government. It is Not applied for the these areas (In case of Yokohama), ・ less than 5 houses ・ the construction for landslide prevention was done
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February 17, 1999 Minami Ward, Yokohama.
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2. Problems in Governmental Organization ・ Bureaus, Departments, and Divisions of government hardly have a cooperation, even if same municipality. ・ They hardly share their data, because their purpose is different.
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Purpose Purpose ・ Make Collaboration
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Joint Research This study is a Joint Research between ・ City of Yokohama Bureau of building Bureau of road Bureau of disaster front office ・ Yokohama National University Tohoku University (Landslide) Tokyo Institute of Technology (Geology)
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Purpose Purpose ・ Propose a new method “how to create a hazard evaluation for landslide in urban area from the Viewpoint as “a Planner”. ・ Utilize “Existing Data”. ・ Make Collaboration
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Data
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25 M DEM
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横浜国立大学
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(1966 ~ 1999)
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Relationship Between Collapse and Slope
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0.00 0.50 1.00 1.50 2.00 2.50 3.00 3.50 4.00 141618202224262830 Calculated Angle (Degree) Number of Collapses / ha Number of Collapses per 1 ha & 1 degree of Calculated Angle Calculated Angle (Degree) Total Collapse Case (%) 0 10 20 30 40 50 60 70 80 90 100 789101112131415161718192021222324252627282930 Ratio of total Collapses per 1 Degree of Calculated Angle (1966 ~ 1999)
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⇒ Actual Angle ≑ 2.5 × Calculated Angle
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Factor of Collapse
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Type 1 Loam Mud Stone Type 2 Mud Stone Face Soil Type 3 Three Major Types of Geological Section in Yokohama Patterns of Geology Patterns of Geology
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+ Records of Collapse Specified Hazard Zone (Prefectural & Municipal) Type 1 Type 2 Type 3 Slump Fall Patterns of Geology Patterns of Collapse
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Hazardous Evaluation for the Risk of Landslide
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A B
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-Distance from cliff -Density of buildings -Structures of buildings -Building use For example, Hospital, Welfare Facilities, etc Consider surrounding environments, as a potential evaluation of suffering form landslide Further Evaluation
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See you next year! Akiyuki Kawasaki Graduate School of Engineering, Yokohama National University, Japan E-mail: akiyuki@arc.ynu.ac.jp URL: http://gisserv.jks.ynu.ac.jp
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Yes No Yes No Yes No
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The problems “Hazard zone for landslide” specified by local government. It is not applied for the these areas, ・ less than 5 houses ・ Apartment ・ The area where the construction for landslide prevention was done
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⇒ Actual Angle ≑ 2.5 × Calculated Angle
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- Propose to Create a New Methodology from the Viewpoint as a “ Planner ”. - Collaborative Project Between Prefectural and Municipal Government and Universities. Summery
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Hazard Evaluation for Landslide Akiyuki Kawasaki, Doctoral Student Graduate School of Engineering, Yokohama National University, Japan
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