摘要
The flow resistance in rivers is an old and partly unsolved problem. In this study, the bed surface fractal dimension（BSFD） is used to describe the bed morphology, and combined with the bed roughness, a general model experiment is developed. The results show that there is a positive relationship between the BSFD and the bed roughness, which can be further applied to estimate the roughness changes in rivers. These findings will also guide further studies of the mobile-bed flow resistance.
The flow resistance in rivers is an old and partly unsolved problem. In this study, the bed surface fractal dimension（BSFD） is used to describe the bed morphology, and combined with the bed roughness, a general model experiment is developed. The results show that there is a positive relationship between the BSFD and the bed roughness, which can be further applied to estimate the roughness changes in rivers. These findings will also guide further studies of the mobile-bed flow resistance.
作者
周银军
卢金友
陈立
任杰
Yin-jun Zhou;Jin-you Lu;Li Chen;Jie Ren(Changjiang River Scientific Research Institute,Wuhan,430010,China;Three Gorges Water Conservancy Complex Cascade Dispatch ＆ Communication Center,Yichang 443000,China;State Key Laboratory of Water Resources and Hydropower Engineering Science,Wuhan University,Wuhan 430072,China;State Key Laboratory Base of Eco-Hydraulic Engineering in Arid Area,Xi＇an University of Technology,Xi＇an 710048,China)
基金
Project supported by the National Natural Science Foundation of China(Grant Nos.51579014,51339001 and 91647117)
the National Key Research and Development of China(Grant No.2016YFC0402301-01)
