| 摘要: |
| 黄河下游河道是黄河流域系统中的一个重要的泥沙沉积汇, 泥沙在这一沉积汇中的沉积对于入海泥沙通量有重要影响。作者引进河道排沙比来表示入海泥沙通量比率, 并以黄河下游实测资料为基础, 运用经验统计方法对入海泥沙通量比率与影响因子的关系进行了研究。入海泥沙通量比率与悬移质中大于0.05mm粗泥沙和小于0.025mm细泥沙的百分比有密切关系, 粗泥沙部分所占比例越高, 则入海泥沙通量比率越低, 而细泥沙所占比例越高, 则入海泥沙通量比率越高。洪水事件中最大含沙量和来沙系数越大, 则入海泥沙通量比率越小。在黄河上、中游的4个水沙来源区中, 两个清水区来水为河道提供了输沙动力, 有助于减小淤积, 有时甚至会发生冲刷, 从而有利于输沙入海, 增加入海泥沙通量比率。两个多沙区的来沙增大了下游河道的输沙负载, 使泥沙容易淤积在河道中, 从而降低入海泥沙通量比率。以年系列和洪水系列资料, 建立了一系列表达上述影响的经验统计关系, 运用这些关系可以解释和预测流域来水来沙及泥沙粒度因子的变化对入海泥沙通量比率变化的影响。研究发现, 近30年来黄河入海泥沙通量比率呈减小趋势。由于黄河下游来水量不断减小, 导致了河床的萎缩和输沙功能的衰退, 使得输送入海的泥沙占下游来沙的比率减小。
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| 关键词: 入海泥沙通量,泥沙输移,黄河 |
| DOI：10.11693/hyhz200306011011 |
| 分类号: |
| 基金项目:中国科学院知识创新工程重要方向项目,KZCX2-20705号及中国科学院地理科学与资源研究所创新项目,CXIOG-A00-05-01号 |
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| SEDIMENT FLUXES TO THE SEA AS INFLUENCED BY SEDIMENT DELIVERY OF THE LOWER YELLOW RIVER |
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XU Jiong-Xin
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Institute of Geographical Sciences and Natural Resources Research, The Chinese Academy of Sciences
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| Abstract: |
| The lower Yellow River in the North China Plain is a large-size sediment sink in the drainage basin. At historical time scales, almost all Quaternary deposits in the North China Plain belonged to this sediment sink; in the modern times, according to the hydrometric data, 400Mt of sediment was deposited in this sink annually, representing 25% of the total annual sediment load of the Yellow River. Thus, sediment deposition in the lower Yellow River plays an essential role in controlling sediment fluxes to the sea. To quantify the effect of this sediment sink, the ratio of sediment flux to the sea to the total sediment inflow of the lower Yellow River (RSF) is studied, on the basis of the data collected at the hydrometric stations. The RSF has been found to decrease with the >0.05 mm percentage in suspended sediment, but increase with the <0.025 mm percentage. Because the sediment carrying capacity of stream flow is lower for coarse fractions of sediment load than for fine ones, therefore, fine sediment has more opportunities to be carried to the sea. The RSF was closely related with the combinations of runoff and sediment; the higher the event maximum suspended sediment concentration and the incoming sediment coefficient were, the lower the RSF. The hyperconcentrated flows also have some influence on the sediment fluxes to the sea. When hyperconcentrated flows occurred, large quantities of sediment may be deposited in the lower Yellow River, especially in the braided reach above Gaocun. Thus, the sediment that could be carried to the sea decreased significantly, leading to a decline in the RSF. This study shows that, when the event maximum suspended sediment concentration was higher than 300kg/m3, the RFS became lower than 0.50. Changes in RSF can be closely related to different water and sediment source areas in the Yellow River drainage basin. Four major runoff and sediment source areas have been identified in the upper and middle Yellow River basin and have different effects on the RSF. The runoff from the two areas where relatively clear runoff is generated may enhance sediment carrying capacity and thereby more sediment is transported to the sea and the RSF increases. On the contrary, the sediment from two major sediment source areas may greatly increase the sediment load of the lower Yellow River, leading to a decreased RSF. Based on the annual and flood-based data, a series of statistical relationships have been established, which may be used to explain and predict the effect induced by the changes in runoff, sediment load and sediment composition. In the past 30 years, the RSF tended to decrease, reflecting the result of channel adjustment in response to the decreasing runoff. Due to the continuously decreased runoff and sediment load to the lower Yellow River, the river channel shrunk and its sediment transporting ability declined. As a result, although the sediment load into the lower Yellow River has shown a tendency of decrease, the sediment deposited in the lower Yellow River does not decrease significantly. This resulted in a decrease in the RSF.
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| Key words: Sediment flux to the sea, Sediment transport, The Yellow River |
