The mechanism of barrier river reaches in the middle and lower Yangtze River

Alluvial channel has always adjusted itself to the equilibrium state of sediment transport after it was artificially or naturally disturbed. How to maintain the equilibrium state of sediment transport and keep the river regime stable has always been the concerns of fluvial geomorphologists. The chan...

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Veröffentlicht in:	Journal of geographical sciences 2017-10, Vol.27 (10), p.1249-1267
Hauptverfasser:	You, Xingying, Tang, Jinwu, Zhang, Xiaofeng, Hou, Weiguo, Yang, Yunping, Sun, Zhaohua, Weng, Zhaohui
Format:	Artikel
Sprache:	eng
Schlagworte:	Alluvial channels Bed load Downstream Earth and Environmental Science Flow Geographical Information Systems/Cartography Geography Nature Conservation Physical Geography Remote Sensing/Photogrammetry Rivers Sediment transport Upstream 下游河段中下游冲积河道扬子江机制水流动力轴线河势稳定纳维-斯托克斯方程
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