A study of the relationship between deposit density and debris flow type
文献类型：会议论文
| 作者 | (1)KANG ZHICHENG; (1)WANG YUZHANG; KANG ZHICHENG
|
| 出版日期 | 1992 |
| 会议日期 | 1992 |
| 会议地点 | Chengdu, China |
| 关键词 | debris flow type deposit density particle component |
| 卷号 | 209 |
| 页码 | 247-252 |
| 通讯作者 | KANG ZHICHENG |
| 英文摘要 | The density of debris flow samples after settling in laboratory (the deposit density) is a kind of limiting density of debris flow, which depends only on the solid component in debris flow including particle composition, size distribution and arrangement. It does not change with the amount of water, This property of deposit density characteristics the type of debris flow. The tendency as well as the reason for change between deposit density and particle component is analysed in the paper. Samples from moving flow in the Jiangjia Ravine near Dongchuan City were obtained and the natural density and deposit density measured. The ratio of natural density to deposit density as a function of debris flow structure, the type and the properties of debris flow ere further researched. |
| 会议录 | Erosion, debris flows and environment in mountain regions
 |
| 会议录出版者 | IAHS |
| 语种 | 英语 |
| ISBN号 | 0-947571-38-8 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/21459]  |
| 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） |
| 通讯作者 | KANG ZHICHENG |
| 作者单位 | Dongchuan Observation and Research Station of Debris Flow, Chinese Academy of Sciences, Chengdu, PO Box 417, Sichuan 610015, China |
| 推荐引用方式 GB/T 7714 | KANG ZHICHENG. A study of the relationship between deposit density and debris flow type[C]. 见:. Chengdu, China. 1992. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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