滑坡型泥石流 | |
康志成![]() | |
专著(文集)名 | 中国科学院兰州冰川冻土研究所集刊 第4号(中国泥石流研究专辑) |
其他责任者 | 中国科学院兰州冰川冻土研究所 |
1985-01 | |
出版者 | 科学出版社 ; 科学出版社 |
出版地 | 北京 ; 北京 |
出处页码 | 171-177 |
出版者 | 科学出版社 ; 科学出版社 |
出版地 | 北京 ; 北京 |
其他题名 | Sliding Debris Flow |
英文摘要 | The sliding debris flow means a movement process beginning with a landslide and ending with a debris flow. Because they occur together and transform quickly, it is difficult to distinguish definitely one from the other. This debris flow belongs to the type of debris flow which is of short-duration and highcreeping with a high velocity and a great density. Wintin a few minutes it can remove hundreds of thousand or even more than ten million of solid material. It carries stones of different size at the rate of a tons of tens per second. Its great destruction is attributed to the shock wave equal to a typhoon of 11 or 12 magnitude besides the debris flow body itself. The cause and properties of this kind of debris flow are illustrated by two example in Yunnan and Sichuan. |
语种 | 中文 |
内容类型 | 专著章节/文集论文 |
源URL | [http://192.168.143.20:8080/handle/131551/4907] ![]() |
专题 | 成都山地灾害与环境研究所_成都山地所知识仓储(2009年以前) 中国科学院水利部成都山地灾害与环境研究所 |
推荐引用方式 GB/T 7714 | 康志成. 滑坡型泥石流. 中国科学院兰州冰川冻土研究所集刊 第4号(中国泥石流研究专辑). 北京, 北京:科学出版社, 科学出版社,1985:171-177. |
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