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Research on Regulation Thoughts for Shoal at Confluence of Xinzhou Channel in the Middle Reach of the Yangtze River

机译:长江中间距离鑫州通道交汇处的调控思想研究

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This paper conducts in-depth discussion to influence factor of shoal's refloating change through analysis. According to analysis, run of upper trench in the Xinzhou south channel and change of north channel's inflow is the major cause of confluence refloating; the article also discusses and illustrates relative thoughts issues in the process of regulating shoal at confluence. Braided reaches prevail in the middle and the lower reaches of the Yangtze River, while navigation obstruction issue at confluence reach is also quite common and complicated. Navigation obstruction refloating of confluence reach is often due to it is jacked by outflow of one branch when water level is high, which forces flow velocity at the other branch of channel slow down. Plus inflow change at both branch channels, sediment deposition and can easily form shoal at confluence of the end of Xinzhou; confluence shoal evolution has much to do with condition adjustment of incoming water and sediment in the upstream besides it is determined by its own pattern. Shoal channel regulation issue at confluence reach is no less complex than estuary reach. It is extremely complicated, therefore, there is an urgent need and it is also imperative to strengthen regulation research on this kind of shoals so as to enhance technological level of regulation.
机译:本文对通过分析进行了深入讨论,以影响浅滩回归改变的因素。根据分析,在鑫州南沟道上进行上部沟渠和北渠道流入的变化是汇合回归的主要原因;本文还讨论并说明了在汇合中调节浅滩过程中的相对思想问题。在长江的中游和下游的编织达到占上风,而汇合达到的导航障碍问题也相当普遍和复杂。汇合达到的导航梗阻往往是由于当水位高时,由于一个分支的流出,这势力在通道的另一个分支中强制流速慢。加上分支频道的流入变化,沉积物沉积,并且可以在鑫州末汇合中轻松形成浅滩;汇合浅滩进化与附带的进入水和沉积物的条件调整有多有关,除了它的上游,它由自己的模式决定。融合达到的浅滩渠道调节问题与河口不那么复杂。这是非常复杂的,因此,迫切需要,加强对这种浅滩的调节研究,以提高调节技术水平。

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