KMS Institute of Mountain Hazards and Environment,CAS
云南盈江浑水沟泥石流与降雨的关系 | |
Alternative Title | The Relation Between Rainfall and Debris Flow in Hunshui Gully, Yingjiang County, Yunnan Province |
Language | 中文 |
刘江; 程尊兰![]() | |
Source Publication | 泥石流(2) |
Editor | 中国科学院成都地理研究所 编辑 |
Pages | 32-35 |
1983 | |
Publisher | 科学技术文献出版社重庆分社 |
Publication Place | 重庆 |
Keyword | 泥石流 降雨 浑水沟 盈江 云南 |
Abstract | The debris flow in Hunshui Gully belongs to the heavy-rainfall-induced one. Standing from real survey datum in three years, the beginning rain intensity causing debris flow in Hunshui Gully is abtained: i(~10)=(123/P(~a)+0.4, mm. Its max. design discharge: Q=1545((0.93i^0.12~1)-1), m^3/s. The hydrograph forms of debris flow have a close bearing on rainfall processes. |
Other Abstract | 本文以1976-1978年浑水沟泥石流、降雨资料为依据,分析了泥石流与降雨的关系。 |
Document Type | 专著章节文集论文 |
Identifier | http://ir.imde.ac.cn/handle/131551/31241 |
Collection | 成都山地所知识仓储(2009年以前) 山地灾害与地表过程重点实验室 |
Affiliation | 中国科学院成都地理研究所 |
Recommended Citation GB/T 7714 | 刘江,程尊兰. 云南盈江浑水沟泥石流与降雨的关系. 泥石流(2). 重庆:科学技术文献出版社重庆分社,1983:32-35. |
Files in This Item: | ||||||
File Name/Size | DocType | Version | Access | License | ||
32-35.pdf(3355KB) | 专著章节文集论文 | 开放获取 | CC BY-NC-SA | View Application Full Text |
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