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首页> 外文期刊>River Research and Applications >FLOW STRUCTURE AND CHANNEL CHANGE IN A SINUOUS GRASS-LINED STREAM WITHIN AN AGRICULTURAL DRAINAGE DITCH: IMPLICATIONS FOR DITCH STABILITY AND AQUATIC HABITAT
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FLOW STRUCTURE AND CHANNEL CHANGE IN A SINUOUS GRASS-LINED STREAM WITHIN AN AGRICULTURAL DRAINAGE DITCH: IMPLICATIONS FOR DITCH STABILITY AND AQUATIC HABITAT

机译:农业排水沟内草形衬里流结构及通径变化:对沟渠稳定性和生境的影响

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Many drainage ditches in the Midwest have developed a geomorphological configuration characterized by vegetated bars, or benches, on the bottom of the ditch and a stream flowing within a channel inset into these bars or benches. Past work has focused on the sedimentology of the benches and the depositional processes involved in bench development. This study investigates the three-dimensional flow structure and short-term channel change in a small grass-lined stream flanked by benches at the bottom of an agricultural drainage ditch in east central Illinois, USA. In particular, it focuses on the influence of channel curvature and bank vegetation on flow through the inset channel at two different stages and explores how the structure of the flow is related to documented patterns of channel change. Results indicate that the mean flow is characterized by a submerged high-velocity core that mainly is confined to the centre of the channel by near-bank zones of flow stagnation/separation induced by abrupt changes in channel alignment and by strong frictional effects of grasses extending into the flow along the channel margins. Where the high-velocity core is close to the channel margins, minor erosional adjustments of the inset channel can occur in the form of bank erosion. Patterns of turbulence kinetic energy reflect the development of shear layers near the channel margins and surrounding the submerged high-velocity core. Locations with strong turbulence also correspond to locations of minor bank erosion. The results indicate that the inset channel is a relatively stable feature, especially where the alignment of this channel is straight, but that erosion-control treatments may be necessary locally where the inset channel impinges on the ditch bank. Although the development of benches, a geomorphic response to ditch maintenance, is commonly viewed as a threat to drainage efficacy, preserving or constructing benches and associated inset channels in drainage ditches can enhance aquatic habitat and water quality.
机译:中西部的许多排水沟已经形成了一种地貌结构,其特征是沟渠底部的植被为条状或长凳,河流在通道中流入这些条状或长凳。过去的工作集中在工作台的沉积学和工作台开发中涉及的沉积过程上。这项研究调查了美国伊利诺伊州中部东部一个农业排水沟底部的一条板凳两侧的小型草丛河流的三维流动结构和短期通道变化。特别是,它着重研究了通道曲率和河岸植被在两个不同阶段对通过插入通道的水流的影响,并探讨了水流的结构与已记录的通道变化模式之间的关系。结果表明,平均流量的特征在于淹没的高速岩心,该高速岩心主要由河道排列的突然变化引起的流动停滞/分离的近岸区和草丛伸展的强烈摩擦作用限制在河道的中心。沿着通道边界流入流量。在高速岩心靠近通道边缘的地方,可以以堤岸侵蚀的形式对插入通道进行较小的侵蚀调整。湍动能的模式反映了通道边缘附近和淹没的高速岩心周围剪切层的发展。湍流强烈的位置也对应于较小的河岸侵蚀位置。结果表明,插入通道是一个相对稳定的特征,特别是在该通道的对齐方式是笔直的情况下,但是当插入通道撞击到沟岸时,可能需要局部进行侵蚀控制处理。尽管长凳的形成是对沟渠维护的一种地貌响应,但通常被视为对排水功效的威胁,但在排水沟中保留或建造长凳和相关的嵌入式通道可以改善水生生境和水质。

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