| Project/Area Number |
12680460
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| Research Category |
Grant-in-Aid for Scientific Research (C)
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| Allocation Type | Single-year Grants |
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| Section | 一般 |
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| Research Field |
Natural disaster science
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| Research Institution | Hirosaki University |
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Principal Investigator |
HIGAKI Daisuke Hirosaki University, Faculty of Agriculture and Life Science, Professor, 農学生命科学部, 教授 (10302019)
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| Co-Investigator(Kenkyū-buntansha) |
YAGI Hiroshi Yamagata University, Faculty of Education, Professor, 教育学部, 教授 (40292403)
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| Project Period (FY) |
2000 – 2003
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| Project Status |
Completed (Fiscal Year 2003)
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| Budget Amount *help |
¥3,400,000 (Direct Cost: ¥3,400,000)
Fiscal Year 2003: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 2002: ¥800,000 (Direct Cost: ¥800,000)
Fiscal Year 2001: ¥1,400,000 (Direct Cost: ¥1,400,000)
Fiscal Year 2000: ¥700,000 (Direct Cost: ¥700,000)
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| Keywords | Himalaya / Nepal / Soil erosion / Bank erosion / River course shifting / Landlslide / Hazard map / Sediment related disaster / 河岸侵食 / 流域管理 / ランドスライド / 地すべり地形 / ハザードマップ |
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| Research Abstract |
This study aims to propose engineering geomorphological investigation points for countermeasure planning against erosion and sedimentation disasters through analysis of present and past geomorphic processes in the Nepal Himalaya
1)By monitoring rate and processes of gully erosion, surface erosion and vegetation recovery for ten years, we evaluated the various adopted countermeasures. Based on it, selecting methods of erosion control measures by investigating stages of gully and rill development is basically conceptualized.
2)Causes of river course widening in the Sub-Himalaya(Siwalik Hills) have been studied through monitoring both erosion of slopes/stream banks and run-off processes as well as geomorphological evolution processes. Extreme flash floods with short tune of run-off concentration have occurred due to dense network of drainage systems due to weak and young geological strata. Huge sediment production from slopes and banks equivalent to the denudation rate of at least 5mm/year in depth is estimated. They are the main causes of river course widening. Land coverage change in a watershed may also be the cause of it.
3)Deep-seated landslide distribution maps have been prepared by aerial photo interpretation in the Lower Himalaya and partly in Sub-Himalaya. It is proposed through the statistical analysis that landslide hazardous slopes can be detected by combination of geology such as lithology and structure and slope angle.
4)A GIS-based landslide hazard zonation method is also proposed from the statistical analysis on the relation between landslide occurrences and then* physiographical attributes.
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