4.6 Article

Morphological adjustments in a meandering reach of the middle Yangtze River caused by severe human activities

期刊

GEOMORPHOLOGY
卷 285, 期 -, 页码 325-332

出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.geomorph.2017.02.022

关键词

Planform geometry; Cross-sectional geometry; Channel adjustments; Human activities; Meandering reach

资金

  1. National Natural Science Foundation of China [51579186, 51339001]
  2. National Key Research and Development Program of China [2016YFC0402303/05]

向作者/读者索取更多资源

In the past 50 years, the Shishou reach in the middle Yangtze River underwent significant channel evolution owing to the implementation of an artificial cutoff, the construction of bank revetment works and the operation of the Three Gorges Project (TGP). Based on the measured hydrological data and topographic data, the processes of channel evolution in this reach were investigated mainly from the adjustments in planform and cross-sectional geometries. The variation in planform geometry obtained in this study indicates that (i) the artificial cutoff at Zhongzhouzi caused the river regime to adjust drastically, with the mean rate of thalweg migration at reach scale of 42.0 m/a over the period 1966-1975; (ii) then the effect of this artificial cutoff reduced gradually, with the mean migration rate decreasing to <30 m/a in 1975-1993, while it increased to >40 m/a owing to the occurrence of high water levels in 1993-1998; and (iii) the average annual rate of thalweg migration decreased to 29.3 m/a because of the impacts of various bank protection engineering and the TGP operation during the period 2002-2015. However, remarkable thalweg migration processes still occurred in local regions after the TGP operation, which resulted in significant bankline migration in local reaches of Beimenkou, Shijiatai, and Tiaoxiankou. In addition, the adjustments of bankfull channel geometry were investigated at section and reach scales after the TGP operation. Calculated results show that lateral channel migration in this reach was restricted by various river regulation works and that channel evolution was mainly characterized by an increase in bankfull depth and cross-sectional area. Empirical relationships were developed between the reach-scale bankfull dimensions (depth and area), the bankfull widths at specified sections, and the previous 5-year average fluvial erosion intensity during flood seasons, with high correlation degrees between them being obtained. (C) 2017 Elsevier B.V. All rights reserved.

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