2010年黄河水沙流量对水沙调控引起的高旋流的响应

Wang Yan, Wang Houjie, Bi Naishuang, Zhang Yong
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引用次数: 2

摘要

水沙调节为黄河口高旋流的观测提供了良好的契机。悬浮物的浓度(SSC)和中位粒径是形成超旋流的重要因素。2010年6月19日第10次水沙整治期间,为研究黄河口水沙流量变化规律,预测黄河口超典型流的形成,在利津站进行了悬沙取样、水深和水流系统测量等同步测量。结果表明:当上游水库开始按期放水时,利津站记录的放水量急剧增加,同时河床侵蚀加剧。大量粗颗粒从河床上重悬,导致水体悬沙浓度(SSC)和含沙量(SL)增加,是粗颗粒悬沙浓度上升的主要原因。后期,在小浪底水库高锥流量的影响下,利津站记录的水量迅速减少,而利津站到河口处的SSC和SL显著增加。细沙浓度的显著增加导致河床淤积严重。由于高SSC和细颗粒浓度是高锥流形成的必要条件,因此可以在河口处预测高锥流过程。高旋流不仅会在短时间内将大量沉积物从河流输送到沿海海域,而且会对河口的地貌和生物地球化学演化产生影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RESPONSE OF WATER-SEDIMENT DISCHARGE OF HUANGHE (YELLOW RIVER)TO THE HYPERPYCNAL FLOW CAUSED BY WATER-SEDIMENT REGULATION IN 2010
The water-sediment regulation provides a good opportunity for the observation of the hyperpycnal flows at the Huanghe(Yellow River)estuary.The concentration(SSC)and median grain size of the suspended sediment are important factors to the formation of hyperpycnal flows.During the 10th watersediment regulation on June 19th,2010,in order to study the variations in water and sediment discharge off the Huanghe River mouth and to predict the formation of hyperypycnal flow,synchronous survey were carried out at the Lijin station,which includes the sampling of the suspended sediment and measurement of the bathymetry and current system.The results suggest that when the reservoirs on the upper reaches of the river started to release water with low suspended sediment concentration(SSC)on schedule,the water discharge recorded at the Lijin station increased sharply,together with the intensification of riverbed erosion.A great amount of the coarser particles were resuspended from the riverbed,resulting in the increase in suspended sediment concentration(SSC)and sediment load(SL)of the water,as the major contributor to the rise of suspended concentration of coarser sediment.In the later stage,under the influence of hyperpycnal discharge off the Xiaolangdi Reservoir,the water discharge recorded at the Lijin station decreased quickly,while the SSC and SL remarkably increased off the Lijin station up to the river mouth.The remarkable increase in fine sediment concentration led to the heavy siltation on the riverbed.It was possible to predict the hyperpycnal process at the river mouth,since both high SSC and fine particles concentration are the necessary requirements for the formation of hyperpycnal flow.The hyperpycnal flow would not only deliver a large amount of sediments from the river to the coastal sea in a short period,but also bring impact to the geomorphological and biogeochemical evolutions of the estuary.
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