基于物理的形态模型的发展,重点是由于冲刷和吸积引起的入射波与瞬态床剖面的相互作用

Y. Cho
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引用次数: 4

摘要

使用动态网格技术开发了基于物理的形态学模型[Seoul Foam],以解释海床(由于淤积和冲刷而发生变形)与入射波浪之间的相互作用。在此过程中,使用了基于Open foam的工具箱OlaFlow作为流体动力学模型。为了验证本研究中提出的基于物理的形态[首尔泡沫],对均匀坡度的海滩上的浅滩过程进行了数值模拟。数值结果表明,成功地模拟了滨前沙坝的形成过程。可以很容易地预测到,沙洲的大小与来袭海浪的性质密切相关,在波涛汹涌的情况下,前海岸的斜坡由于冲刷而迅速变形。在温和海中,海岸线附近形成了几个沙波,在暴露时间相同的情况下,沙波的大小没有风浪大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of Physics-Based Morphology Model with an Emphasis on the Interaction of Incoming Waves with Transient Bed Profile due to Scouring and Accretion using Dynamic Mesh
A physics-based morphology model [Seoul Foam] was developed using the dynamic mesh technique to explain the interaction between the sea bed, which undergoes deformation due to siltation and scouring, and the incoming waves. In doing so, OlaFlow, an Open Foam-based toolbox, was used as a hydrodynamic model. To verify the proposed physically-based morphology [Seoul Foam] in this study, numerical simulations of the shoaling process over the beach of the uniform slope were implemented. The numerical result shows that the formation process of a sand bar over the foreshore was successfully simulated. As can be easily anticipated, the size of the sand bar was closely linked to the nature of incoming waves, and in the case of a rough sea, the foreshore slope was rapidly deformed due to scouring. In mild seas, several sand waves were formed near the shoreline, and when the exposure time was the same, the size of the sand waves was not as large as in rough seas.
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