首页> 外文期刊>Journal of applied mathematics >A Coupled Model of the 1D River Network and 3D Estuary Based on Hydrodynamics and Suspended Sediment Simulation
【24h】

A Coupled Model of the 1D River Network and 3D Estuary Based on Hydrodynamics and Suspended Sediment Simulation

机译:基于水动力和悬浮泥沙模拟的一维河网与三河口耦合模型

获取原文
           

摘要

River networks and estuaries are very common in coastal areas. Runoff from the upper stream interacts with tidal current from open sea in these two systems, leading to a complex hydrodynamics process. Therefore, it is necessary to consider the two systems as a whole to study the flow and suspended sediment transport. Firstly, a 1D model is established in the Pearl River network and a 3D model is applied in its estuary. As sufficient mass exchanges between the river network and its estuary, a strict mathematical relationship of water level at the interfaces can be adopted to couple the 1D model with the 3D model. By doing so, the coupled model does not need to have common nested grids. The river network exchanges the suspended sediment with its estuary by adding the continuity conditions at the interfaces. The coupled model is, respectively, calibrated in the dry season and the wet season. The results demonstrate that the coupled model works excellently in simulating water level and discharge. Although there are more errors in simulating suspended sediment concentration due to some reasons, the coupled model is still good enough to evaluate the suspended sediment transport in river network and estuary systems.
机译:河网和河口在沿海地区非常普遍。在这两个系统中,来自上游的径流与来自公海的潮流相互作用,导致复杂的流体动力学过程。因此,有必要将两个系统作为一个整体来研究水流和悬浮泥沙的运移。首先,在珠江网络中建立一维模型,并在其河口中应用3D模型。由于河网与其河口之间有足够的质量交换,因此可以采用界面处水位的严格数学关系来将1D模型与3D模型耦合。这样,耦合模型不需要具有公共的嵌套网格。河网通过在界面处增加连续性条件,将悬浮的泥沙与其河口交换。耦合模型分别在干燥季节和潮湿季节进行校准。结果表明,该耦合模型在模拟水位和流量方面表现出色。尽管由于某些原因在模拟悬浮泥沙浓度方面存在更多错误,但耦合模型仍然足以评估河流网络和河口系统中的悬浮泥沙传输。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号