Impact of water diversion on the morphological development of the Lower Yellow River

• 作 者: Huib J. de VRIEND
• 机 构: Delft University of Technology Faculty of Civil Engineering and Geosciences,,Director Science and T
• 出 处: International Journal of Sediment Research
• 发表日期: 2008年01期
• 关键词: Lower morphological river downstream Yellow upstream sedimentation Sediment Dist

In this paper we carry out a theoretical analysis based on the general one-dimensional morphodynamic model for rivers in order to show how the morphological equilibrium of a river is influenced by water and sediment diversion/supply along the river. The results of the analysis show that large scale water diversions, like those along the Lower Yellow River, can cause the development of a convex riverbed profile in the long-term. Deposition will take place along the whole reach of the river, with an increasing deposition depth from downstream to upstream. The slope of the river bed increases from upstream to downstream. Furthermore, an analysis on the morphological time scale shows that this development in the Lower Yellow River will take a time period on the order of decades to centuries. The results of the analysis have been compared with observations in the Lower Yellow River. Since the second half of the 1980’s large scale water diversions from the Yellow River have been taking place. The observations show that this has indeed led to significant sedimentation along the river.

In this paper we carry out a theoretical analysis based on the general one-dimensional morphodynamic model for rivers in order to show how the morphological equilibrium of a river is influenced by water and sediment diversion / supply along the river. that large scale water diversions, like those along the Lower Yellow River, can cause the development of a convex riverbed profile in the long-term. Deposition will take place along the whole reach of the river, with an increasing deposition depth from downstream to upstream . The slope of the river bed increases from upstream to downstream. An analysis of the morphological time scale shows that this development in the Lower Yellow River will take a time period on the order of decades to centuries. The results of the analysis have been compared with observations in the Lower Yellow River. Since the second half of the 1980’s large scale water diversions from the Yellow River have been taking place The observations show that this has indeed led to significant sedimentation along the river.