黄河下游游荡段畸形河势的时空分布及演变规律

Spatiotemporal distribution and evolution of abnormal river regimes in the braided reach of the Lower Yellow River

  • 摘要: 1985年以来黄河下游游荡段畸形河势频发,为科学治理黄河增加了难度。本文采用深度学习方法精准解译遥感影像,结合历史数据资料,系统研究了黄河下游游荡段1985—2023年畸形河势的时空分布,重点分析了游荡段上段、中段和下段的3个典型畸形河势河段的演变过程。为了定量表示主流偏离治导线的程度,提出了偏离规划度的概念,然后从局部河段、单个河湾和断面3个尺度的形态变化分析了游荡段畸形河势的演变规律。研究结果表明:小浪底水库运行后畸形河势位置发生了上移,目前多发生在游荡段上段;枯水多沙条件易形成畸形河势;偏离规划度小于0.2的河段不会发生畸形河势;畸形河势的发展受到河床质的影响,裁弯会从深泓点开始冲刷,并不断往两侧发展。本研究成果可为科学治理黄河下游游荡段提供参考依据。

     

    Abstract: The frequent abnormal river regimes in the braided reach of the Lower Yellow River since 1985 have significantly complicated rational management of the Yellow River. This study aims to characterize the spatiotemporal distribution and evolution laws of abnormal river regimes in the braided reach of the Lower Yellow River from 1985 to 2023. Deep learning methods were applied to historical remote sensing images to identify the changes to the three typical abnormal river sections in the upper, middle, and lower reaches of the braided segment. A novel approach, Deviation degree from the proposed river alignments (DD), was introduced to quantitatively assess the degree of deviation of the mainstream from the proposed river alignments, following which the evolution of abnormal river regimes was examined at three morphological scales: local river sections, individual river bends, and cross-sections. The results show that operationalization of the Xiaolangdi Reservoir has shifted the locations of abnormal river regimes upstream, predominantly in the upper section of the braided reach. Abnormal regimes are more likely to develop under low-flow and high-sediment conditions. River sections with a DD < 0.2 will not develop abnormal regimes. Riverbed material influences the evolution of abnormal river regimes, with the cut-off of abnormal river bends initiating scouring at the deepest river point, which subsequently progressively expands laterally. The outcomes of this study can guide improved scientific management of the braided reach of the Lower Yellow River.

     

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