Morphologic evolution of bifurcated reaches in a macrotidal estuary with mountain streams  

作　　者：Jing Liu Yongjun Lu Liqin Zuo Huaixiang Liu Qun Xu Qingzhi Hou 

机构地区：[1]State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Nanjing Hydraulic Research Institute,Nanjing 210024,China [2]Department of College of Water Conservancy and Hydropower Engineering,Hohai University,Nanjing 210098,China [3]Yangtze Institute for Conservation and Development,Nanjing 210098,China

出　　处：《International Journal of Sediment Research》2022年第6期857-870,共14页国际泥沙研究（英文版）

基　　金：The current study was financially supported by the National Natural Science Foundation of China(NSFC,Grant Nos.52071221 and U2040219)。

摘　　要：A macrotidal estuary with mountain streams(MEMS)is characterized by rapidly rising and falling flood peaks and large tidal ranges and is a typical estuary type with strong flow dynamics that is found worldwide.Understanding the morphodynamic evolution of MEMSs has great significance for river management.The roles of the mountain stream river flood process and macrotides on the morphology evolution still needs further quantitative study.Taking the Oujiang Estuary as an example,the evolution mechanisms of bifurcated reaches of a MEMS are studied by analyzing the hydrologic and topographic data and using a two-dimensional numerical model for flow-sediment transport.The results show that(1)under the combined actions of runoff and macrotides,sediment transport is active and morphological evolution is intensive,the main branch and subbranch historically switch frequently,and erosion generally occurs in wet years,while deposition occurs in dry years.(2)The river flood process of mountain streams causes rapid erosion,which rises and falls rapidly with a kurtosis index(K)of approximately 2.9.There is a logarithmic relation between the sediment transport load and K.The volume of sediment transport will be 40%larger than the river flood process with K=1.2 as for the Yangtze River.(3)Macrotides with large tidal ranges could enhance the discharge asymmetry(ψ).When the ψ is greater than 1,the side branches are dominated by flood tides.Although the current study is site specific,the results are expected to provide a valuable reference for sustainable management in similar estuaries.

关 键 词：Mountain stream Macrotide Kurtosis index of river flooding Tide asymmetry Morphological evolution Bifurcated reach 

分 类 号：TV148[水利工程—水力学及河流动力学]