中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Influence of Flow Width on Mean Velocity of Debris Flows in Wide Open Channel

文献类型:期刊论文

作者Kaiheng Hu; Yong Li
刊名Journal of Hydraulic Engineering
出版日期2013
卷号139期号:1页码:65–69
关键词Debris flows Manning resistance coefficient Mean flow velocity Flow width
通讯作者Kaiheng Hu
英文摘要

Debris flow in a wide open downstream channel has a significant transverse velocity component that strongly influences its mean longitudinal velocity. Investigation of observation data of debris-flow surges at Jiangjia Ravine in China shows the dependency of Manning resistance of debris flows on the ratio of flow width to depth. Regression fit reveals a power function relationship between the Manning resistance coefficient and the width-to-depth ratio. This derives a new formula of mean velocity incorporating the influence of flow width. The result indicates that the width-to-depth ratio can be viewed as a kind of shape roughness analogous to grain roughness in the Darcy-Weisbach resistance coefficient expression.




Read More: http://ascelibrary.org/doi/abs/10.1061/%28ASCE%29HY.1943-7900.0000648

Debris flow in a wide open downstream channel has a significant transverse velocity component that strongly influences its mean longitudinal velocity. Investigation of observation data of debris-flow surges at Jiangjia Ravine in China shows the dependency of Manning resistance of debris flows on the ratio of flow width to depth. Regression fit reveals a power function relationship between the Manning resistance coefficient and the width-to-depth ratio. This derives a new formula of mean velocity incorporating the influence of flow width. The result indicates that the width-to-depth ratio can be viewed as a kind of shape roughness analogous to grain roughness in the Darcy-Weisbach resistance coefficient expression.




Read More: http://ascelibrary.org/doi/abs/10.1061/%28ASCE%29HY.1943-7900.0000648

Debris flow in a wide open downstream channel has a significant transverse velocity component that strongly influences its mean longitudinal velocity. Investigation of observation data of debris-flow surges at Jiangjia Ravine in China shows the dependency of Manning resistance of debris flows on the ratio of flow width to depth. Regression fit reveals a power function relationship between the Manning resistance coefficient and the width-to-depth ratio. This derives a new formula of mean velocity incorporating the influence of flow width. The result indicates that the width-to-depth ratio can be viewed as a kind of shape roughness analogous to grain roughness in the Darcy-Weisbach resistance coefficient expression.




Read More: http://ascelibrary.org/doi/abs/10.1061/%28ASCE%29HY.1943-7900.0000648
Debris flow in a wide open downstream channel has a significant transverse velocity component that strongly influences its mean
longitudinal velocity. Investigation of observation data of debris-flow surges at Jiangjia Ravine in China shows the dependency of Manning resistance of debris flows on the ratio of flow width to depth. Regression fit reveals a power function relationship between the Manning resistance coefficient and the width-to-depth ratio. This derives a new formula of mean velocity incorporating the influence of flow width. The result indicates that the width-to-depth ratio can be viewed as a kind of shape roughness analogous to grain roughness in the Darcy-Weisbach resistance coefficient expression.
语种英语
公开日期2013-01-29
源URL[http://192.168.143.20:8080/handle/131551/4854]  
专题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
推荐引用方式
GB/T 7714
Kaiheng Hu,Yong Li. Influence of Flow Width on Mean Velocity of Debris Flows in Wide Open Channel[J]. Journal of Hydraulic Engineering,2013,139(1):65–69.
APA Kaiheng Hu,&Yong Li.(2013).Influence of Flow Width on Mean Velocity of Debris Flows in Wide Open Channel.Journal of Hydraulic Engineering,139(1),65–69.
MLA Kaiheng Hu,et al."Influence of Flow Width on Mean Velocity of Debris Flows in Wide Open Channel".Journal of Hydraulic Engineering 139.1(2013):65–69.

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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