云南盈江浑水沟泥石流与降雨的关系

IMHE OpenIR > 成都山地所知识仓储（2009年以前）

	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.

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