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STUDY ON 1D AND 2D COUPLING FLOW AND SALINITY MODEL AT YANGTZE RIVER ESTUARY

机译:长江口的1D和2D耦合流量和盐度模型研究

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摘要

1-D and 2-D coupling flow and salinity mathematical was established in this paper, in which Datong to Jiangyin reach was simulated by 1-D model and downstream Jiangyin simulated by 2-D model respectively. 1-D river-net mathematical model and 2-D horizontal mathematical model in generalized curvilinear coordinate are was established respectively, and then 1-D and 2-D model were coupled. The established 1-D and 2-D model was calibrated by field datum from Datong to Jiangyin reach and downstream Jiangyin, the calculated results was found agreeable with exact results, which verified established model's reliability and the model can be used to simulate the rules of flow and salinity at Yangtze River Estuary.
机译:本文建立了1-D和2-D耦合流动和盐度数学,其中大同于江阴达到的二维模型和下游江阴分别模拟2-D型模型。 分别建立了1-D河网数学模型和2-D水平数学模型,分别建立了1-D和2-D模型。 已建立的1-D和2-D模型由大同到江阴到江阴的实地基准校准,江阴下游,计算结果与确切的结果相吻合,验证了既定的模型的可靠性,该模型可用于模拟规则 长江口的流动和盐度。

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