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Daily Bank Erosion Rates in the Lower Yellow River Before and After Dam Construction
Authors:Junqiang Xia  Tao Li  Xiaojuan Li  Xiaolei Zhang  Quanli Zong
Institution:1. State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, , Wuhan, 430072 China;2. Yellow River Institute of Hydraulic Research, Yellow River Conservancy Commission, , Zhengzhou, 450003 China
Abstract:During the period of water impoundment and sediment detention of the Sanmenxia Reservoir, riverbank erosion processes played a key role in the channel evolution of the Lower Yellow River (LYR). However, research into bank erosion rates of the LYR has been neglected due to the lack of direct field monitoring. In this study, an indirect method is proposed to determine bank erosion rates at daily time scales by outlining a detailed calculation procedure using measured hydrological data. A total of 810 data points of daily bank erosion rates before and after the construction of Sanmenxia Dam was calculated at seven hydrometric sections along the LYR, with the corresponding values of the bank stability coefficient and the width‐to‐depth ratio also being calculated. Empirical relations were then developed to estimate the daily bank erosion rates, using these parameters at the sections. Temporal and spatial variability in daily bank erosion rates in the LYR before and after dam construction were also investigated, revealing that: (1) the bank erosion rates had a mean value of 16.7‐29.1 m/day in the braided reach, with a maximum value of 290.0 m/day, while they were relatively low in the meandering reach, with a mean value of 2.5 m/day; (2) the erosion rates before dam construction were slightly greater than those after dam construction, with the difference reaching 5‐10 m/day in the braided reach, decreasing in the transitional reach gradually, and being slight in the meandering reach.
Keywords:bank erosion  daily erosion rate  bank stability coefficient  braided reach  meandering reach  dam construction  Lower Yellow River
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