首页> 外文期刊>Journal of Hydrology >Effects of Three Gorges Dam operation on spatial distribution and evolution of channel thalweg in the Yichang-Chenglingji Reach of the Middle Yangtze River, China
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Effects of Three Gorges Dam operation on spatial distribution and evolution of channel thalweg in the Yichang-Chenglingji Reach of the Middle Yangtze River, China

机译:三峡水坝运作对宜昌 - 成岭县宜昌河畔泰尔中的空间分布及演化的影响

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The evolution of the channel thalweg and pool-riffle sequences is a critical feature of morphological adjustments in fluvial systems and might have important effects on aquatic habitat quality, channel stability and navigation. Based on the 220 cross-sectional profiles from 2002 to 2016, residual depths and spatial statistical analyses were used to quantitatively analyse the vertical variations and longitudinal distribution of the pool-riffle sequences and channel thalweg in the Yichang-Chenglingji Reach (YCR) of the Middle Yangtze River, which consists of the Yizhi-Zhijiang, Shashi-Gongan and Shishou-Jianli sub-reaches. The results showed that the dramatic reduction in the sediment loads following the construction of the Three Gorges Darn (TGD) has caused significant adjustments in the size, morphological diversity and spatial distribution of pool-riffle structures in the YCR. The average depth of the pools in the Yizhi-Zhijiang Reach and the Shishou-Jianli Reach overall exhibited a nonlinear growth trend, with the average residual depth increasing by 1.4 m and 1.9 m, respectively. However, the average residual depth in the Shashi-Gongan Reach showed a decreasing trend, with a reduction of approximately 1.2 m. The longitudinal lengths of the riffles in all three reaches contracted to different degrees, and the specific percentage of longitudinal river length occupied by riffles (total riffle length/total sub-reach length) decreased by 8%, 9.6% and 5.9% in the three sub-reaches from upstream to the downstream. In addition, the morphological diversity of the thalweg elevation in the Shashi-Gongan Reach and Shishou-Jianli Reach weakened after the construction of the TGD, while the bed topography in the Yizhi-Zhijiang Reach became more complex and diverse. Moreover, the pool-riffle structures in the YCR were rearranged and distributed regularly following the initiation of the TGD operation, although the variation characteristics of the average pool spacing in the three
机译:通道Thalweg和池 - Riffle序列的演变是河流系统形态调整的关键特征,可能对水生栖息地质量,信道稳定性和导航具有重要影响。基于2002年至2016年的220个横截面型材,使用残余深度和空间统计分析来定量分析尤基 - 成欣达(YCR)中池 - Riffle序列和通道Thalweg的垂直变化和纵向分布中年长江,由伊智 - zh江,施希南和石狮剑力亚达组成。结果表明,三峡(TGD)建设后沉积物载荷的剧烈减少导致YCR在YCR中池 - Riffle结构的尺寸,形态多样性和空间分布的显着调整。 Yizhi-Zhijiang Reach和Shishou-Jianli达到整体池的平均深度表现出非线性增长趋势,平均剩余深度分别增加1.4米和1.9米。然而,Shashi-Gongan Arth的平均剩余深度显示出降低趋势,减少约1.2米。所有三个达抗冲击率的纵向长度缩小到不同程度,纵向河流长度的特定百分比(浅滩长度/总升级长度)下降了8%,9.6%和5.9%从上游到下游的子到达。此外,南宫伸出的丘陵高度的形态多样性达到了施工后的TGD后疲软,而Yizhi-Zhijiang的床上地形变得更加复杂和多样化。此外,在TGD操作开始后,YCR中的池 - Riffle结构被重新排列并定期分布,尽管三个平均池间距的变化特性

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