自由漂浮的大型植物根冠层的平均和湍流结构观测

Maureen A. Downing-Kunz, Mark T. Stacey
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引用次数: 22

摘要

自由漂浮的大型植物通常生长在密集的草席中,它们的羽毛状、不固定的根在水面形成树冠,会影响溪流的水力学和水质。为了更好地了解自由漂浮的大型植物根冠层的水动力效应,本研究考察了一种常见的自由漂浮的大型植物水葫芦(Eichhornia crassipes)与周围水流之间的物理相互作用。在明渠流室中进行了通过和围绕根冠的流场实验。通道中根冠层的存在引起了周围水流的偏转,降低了冠层内的流速。在冠层长度的50%以上观察到增加的雷诺应力和湍流动能,最终在下游的大尾迹区域达到高潮。超过50%冠层长度的平均流速垂直剖面出现拐点,表明混合层的发育类似于陆生和水生植被的叶冠层混合层。垂直湍流结构表现为扫掠、相干涡和沿冠层边缘的混合效率提高。虽然根冠层外湍流混合增加,但根冠层与开放水域之间的湍流交换有限。这意味着穿过冠层-水界面的动量通量较低,因此我们预计在根冠层的停留时间主要是水平平流。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Observations of mean and turbulent flow structure in a free-floating macrophyte root canopy

Observations of mean and turbulent flow structure in a free-floating macrophyte root canopy

Free-floating macrophytes often grow in dense mats, and their feathery, unanchored roots form canopies at the water surface that can affect stream hydraulics and water quality. This study examines the physical interactions between a common species of free-floating macrophyte, water hyacinth (Eichhornia crassipes), and surrounding water flow to better understand the hydrodynamic effects of free-floating macrophyte root canopies. Experiments in an open-channel flow chamber were conducted to examine flow fields through and around root canopies. The presence of the root canopy in the channel caused deflection of flow around and reduced velocities within the canopy. Increased Reynolds stress and turbulent kinetic energy were observed beyond 50% of canopy length, culminating in a large wake region immediately downstream. Vertical profiles of mean streamwise water velocity beyond 50% of canopy length exhibited inflection points, suggesting mixing layer development analogous to mixing layers in leaf canopies of terrestrial and aquatic vegetation. The vertical turbulent structure exhibited sweeps, coherent vortices, and increased mixing efficiency along the canopy edge. Although turbulent mixing increased outside the root canopy, limited turbulent exchange between the root canopy and the open water was observed. This implies low momentum flux across the canopy–water interface, and therefore we expect residence time in the root canopy to be dominated by horizontal advection.

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