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A 2D finite volume simulation tool to enable the assessment of combined hydrological and morphodynamical processes in mountain catchments

机译:2D有限卷仿真工具,以便在山地集水区中的组合水文和形态学过程进行评估

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摘要

Nowadays, the great power of modern computers allows to develop computational models able to deal with simulations of several coupled phenomena over detailed complex topography. An efficient and properly calibrated computational model represents a useful tool to provide insight into the catchment dynamics at hydrological and geomorphological levels. In addition, it allows to develop detailed risk management and conservation plans. In this work, we present a coupled surface-groundwater distributed flow model with hydrological (rainfall and infiltration) and geomorphological (suspended and bed load sediment transport) components. The coupled model is applied to well characterized experimental catchments that are used as realistic test cases. The calibration of the water flow model response to rainfall is performed by means of the fitting to experimental outlet hydrographs of the results supplied by a coupled formulation of 2D Shallow Water Equations and 2D Darcy's law for saturated porous media connected via suitable infiltration laws. The calibration of a suspended and bed load model is also addressed by means of the fitting to experimental outlet sedigraphs. The numerical results show a good agreement between numerical and observed hydrographs and sedigraphs, significantly improving previous published simulations. Additionally, the need to repeat the simulations in the calibration processes is no longer an unapproachable problem.
机译:如今,现代计算机的强大力量允许开发能够在详细复杂地形上处理多个耦合现象的计算模型。一种有效且适当校准的计算模型代表了一种有用的工具,可以在水文和地貌水平处提供进入集水动态的洞察力。此外,它还允许制定详细的风险管理和保护计划。在这项工作中,我们介绍了一种耦合的表面地下水分布式流动模型,具有水文(降雨和渗透)和地貌(悬浮和床荷兰传输)组分。耦合模型应用于良好的特征实验集水区,其用作现实测试用例。通过适用于由2D浅水方程和2D达西对饱和多孔介质的耦合制剂提供的结果的实验​​出口水文的实验出口水文的实验出口水文进行校准,对通过合适的渗透法连接的饱和多孔介质提供的结果。悬浮和床载模型的校准也通过适配的实验出口墓地解决。数值结果表明了数值和观察的文文照片和遗址之间的良好一致性,显着改善了以前发表的模拟。此外,在校准过程中重复模拟的需要不再是一个不可用的问题。

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