1988 Fiscal Year Final Research Report Summary
Comparative study of the large-scale landslides in the Zhangjian and the Hwang Ho Valleys.
| Project/Area Number |
63043025
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| Research Category |
Grant-in-Aid for Overseas Scientific Research
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| Allocation Type | Single-year Grants |
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| Section | Field Research |
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| Research Institution | Niigata University |
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Principal Investigator |
AOKI Shigeru Professor of the Research Institute for Hazards in Snowy Areas, Niigata University, 積雪地域災害研究センター, 教授 (80018621)
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| Co-Investigator(Kenkyū-buntansha) |
王 蘭生 成都地質学院, 応用地質学科, 教授
張 倬元 成都地質学院, 応用地質学科, 教授
SATO Osamu Assistant Professor of the Research Institute for Hazards in Snowy Areas, Niigat, 積雪地域災害研究センター, 助教授 (00022624)
KAWAKAMI Hiroshi Professor of Civil Engineering, Department of Technology, Shinshu University., 工学部, 教授 (00020967)
ENDO Jiro Professor of Forestry, Department of Agriculture, Niigata University., 農学部, 教授 (70007087)
ZHUAN Zhuoyuan Professor of Engineering Geology, Chengdu College of Geology.
LONG Xueming Assistant Professor of Engineering Geology, Chengdu College of Geology.
WANG Lanshen Professor of Engineering Geology, Chengdu College of Geology.
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| Project Period (FY) |
1988
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| Keywords | Landslide / Debris slide / Rock slide / Primary slide / 日中地すべりの比較 |
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| Research Abstract |
Joint investigation have been carried out in the landslides and debris flows in Niigata and Nagano Prefectures in October 1-21, 1988 continued to joint works with Chinese scientists in China. The obtained results from these works can be summarized as follows:
1. The investigated and reported landslides in Japan are reactivated debris slides, whereas the landslides in China are divided into two types, limestone or dolomite rock slides and reactivated debris slides. The investigation of rock slides in China may contribute to Understanding the sliding mechanism of primary landslides which are rarely observed in Japan, recently,
2. The storms are the main cause for occurrence of debris slides in China which did damage to human lives, houses, et ct.. It is characteristic feature that the snow-melting water as well as heavy rains acts as trigger of sliding in northern Japan.
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Research Products
(8 results)
