IMHE OpenIR  > 成都山地所知识仓储(2009年以前)
Thesis Advisor徐俊名
Degree Grantor中国科学院成都山地灾害与环境研究所
Place of Conferral成都
Degree Name硕士
Degree Discipline自然地理学
Other AbstractThis paper discussed the cause and the characteristics of debris flow at Hailuogou in Mt, Gangga. 1) The mountain environment in Hailuogou is very complex Both all natural component and their constitutal relations have the clear feature of the vertical zonality. 2) There are sufficient solid Materials, steep slope and large vertical gradient of gully in Hailuogou Debris flow will break out so long as it is excitated by outside force. 3) Formation precess of debris flow can be summarized two types which are transport and slip meanwhile debris flow can be simulated by catastrophe model as it has catastrophe nature. 4) Debris flow have the characteristics of wave motion boulder bore on boulder and across gully stone beach in accumulation. 5) Debris flow have complete types and zontility distribution. 6) We must do countermeasure seeing that debris flow have influenced the developing Hailougou.
Document Type学位论文
Recommended Citation
GB/T 7714
赵健. 贡嗄山海螺沟泥石流成因与特征研究[D]. 成都. 中国科学院成都山地灾害与环境研究所,1990.
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