中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
云南盈江浑水沟泥石流流速计算

文献类型:专著章节文集论文

语种中文
作者刘江; 程尊兰
发表日期1981-12
页码87-89
出版者科学技术出版社重庆分社
出版地重庆
关键词泥石流 流速计算 浑水沟 盈江 云南
交替题名Velocity Calcuation of Debris Flow in Hunshui Gully, Yingjiang, Yunnan
英文摘要The viscosity of flow causes energy loss when flow is in motion. Although the viscosity of debris flow can not be surveyed directly to to now, it may be shown indirectly by the volume weight of debris flows and the effective viscosity of the slurry of debris flows. The debris flows pattens in Hunshui Gully belong to turbulent flow. Thus, the calculation of their velocity can be done with the help of the formula for turbulent flow velocity (Chezy--Manning Formula). By comparing the velocity of debris flows with the velocity of water flow, and analysing the relation between them on the basis of the data of actual observation and test in a simple wooden flute, the formula of the velocity of debris flows in Hunshui Gully is obtained.Vc=(μ/μcd)^0.1*(γ/γc)^0.4*V, in which Vc is velocity of debris flows, V is velocity of water flow, μ is dynamic viscosity factor of water, μcd is effective viscosity of debris flow slurry, γ is volume weight of water, and γc volume weight of debris flows.
源URL[http://ir.imde.ac.cn/handle/131551/26991]  
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)
成都山地灾害与环境研究所_山地灾害与地表过程重点实验室
作者单位中国科学院成都地理研究所
推荐引用方式
GB/T 7714
刘江,程尊兰. 云南盈江浑水沟泥石流流速计算. 重庆:科学技术出版社重庆分社,1981:87-89.

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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