论文标题

森林密度比树木的刚性更有效地减少海啸的陆上能量通量:来自大型涡流的证据,具有流体结构相互作用

Forest density is more effective than tree rigidity at reducing the onshore energy flux of tsunamis: Evidence from Large Eddy Simulations with Fluid-Structure Interactions

论文作者

Mukherjee, Abhishek, Cajas, Juan Carlos, Houzeaux, Guillaume, Lehmkuhl, Oriol, Suckale, Jenny, Marras, Simone

论文摘要

世界各地的社区对基于自然的解决方案对缓解沿海森林等沿海风险的解决方案越来越感兴趣,但尚不清楚植被提供了多少保护效益,尤其是在海啸影响后的高能性流量的极限上。当前的研究使用三维不可压缩的计算流体动力学模型采用流体结构相互作用方法,旨在量化能量反射和耗散如何随沿海森林的刚性和植被密度而变化。 我们将树干表示为圆柱体,并使用硬木树(如松木或橡木)的弹性模量来表征这些圆柱体的刚性。数值结果表明,能量反射仅对单个气缸的刚度增加。在存在多个圆柱体的情况下,随着圆柱数量的增加,刚度变化而产生的能量反射差异会降低。我们发现,由多个树干的存在造成的阻滞区域主导了能量反射。由于树干被流体动力变形,它们会改变它们周围的流场,从而导致尾流区域的湍流动能产生。结果,树木消散流动能量,突出沿海森林通过反射和散发量减少海啸的陆上能量通量。

Communities around the world are increasingly interested in nature-based solutions to mitigation of coastal risks like coastal forests, but it remains unclear how much protective benefits vegetation provides, particularly in the limit of highly energetic flows after tsunami impact. The current study, using a three-dimensional incompressible computational fluid dynamics model with a fluid-structure interaction approach, aims to quantify how energy reflection and dissipation vary with different degrees of rigidity and vegetation density of a coastal forest. We represent tree trunks as cylinders and use the elastic modulus of hardwood trees such as pine or oak to characterize the rigidity of these cylinders. The numerical results show that energy reflection increases with rigidity only for a single cylinder. In the presence of multiple cylinders, the difference in energy reflection created by varying rigidity diminishes as the number of cylinders increases. Instead of rigidity, we find that the blockage area created by the presence of multiple tree trunks dominates energy reflection. As tree trunks are deformed by the hydrodynamic forces, they alter the flow field around them, causing turbulent kinetic energy generation in the wake region. As a consequence, trees dissipate flow energy, highlighting coastal forests reducing the onshore energy flux of tsunamis by means of both reflection and dissipation.

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