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Research of Sedimentation Model and Waterway Transit Capacity Improvement in the Three Gorges Reservoir
YANG Shengfa, LI Wenjie, HU Xiaoqing, HU Jiang, WANG Tao
2016, 35(S1):
41-48.
DOI: 10.3969/j.issn.1674-0696.2016.sup1.06
After ten years’ operation,the actual sedimentation in the Three Gorges Reservoir (TGR) shows quite a difference from that estimated in demonstration phases due to the changes of incoming flow and sediment, which shows a great need improving its waterway transit capacity. The total sedimentation in the TGR is about 1.5 billion tons, which is mainly distributed at the wide and bend reaches in the permanent backwater region, and no cumulative sedimentation exists in the gorges, and the median particle diameter of the sedimentation is less than 0.01mm. Sedimentation of pebble is concentrated in the fluctuating backwater area, but the deposition amount is relatively small. Navigation obstacles caused by suspended sedimentation have taken place at Huanghuacheng waterway in permanent backwater region owing to the occurrence of bed load movement at some waterways in the fluctuating backwater area during the falling stage. Based on field measurements, mathematical models and physical models, a sedimentation model is proposed in the TGR, and has been successfully applied in the mathematical model and physical model of Huanghuacheng waterway. Based on the two-dimensional water-sediment mathematical model, it is concluded that the retrogressive sedimentation will be less than that expected, facilitating the waterway transit capacity improvement in fluctuating backwater area, and a preliminary treatment is put forward for the construction of the ‘4.5m-deep waterway’.
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