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The influence of meander bend evolution on the formation of multiple cutoffs: findings inferred from floodplain architecture and bend geometry

机译:弯曲弯道演变对多个截止的形成的影响:从洪泛区建筑和弯道几何结构推断出的发现

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The evolution of meander bends and formation of cutoffs, including a series of cutoffs developed simultaneously in a number of bends, have been investigated by many researchers. However, relatively little is known about factors that lead to the development of multiple cutoffs that are formed subsequently at one location. The present study aims to determine the influence of meander bend development on multiple chute cutoff formation in a single bend. The research is based on the sedimentary record of meander migration and cutoffs preserved in a lowland river floodplain (the lower Obra River, Poland). Analysis of changes in meander geometry was conducted to describe the influence of their migration on cutoff formation and in other rivers where multiple cutoffs occurred. The results showed that multiple cutoffs in the lower Obra River have occurred during the last 3000years, owing to the interaction of upstream and downstream controls: migration of meander bends in opposing directions accompanied by an increase of flood frequency and sediment supply. The flow and sediment supply has been further altered since the nineteenth century due to anthropogenic impacts: an artificial cutoff of the downstream bend and elevation of channel levees. Similar mechanisms driving the formation of multiple cutoff have been found in other river courses, despite significantly higher energy of the compared rivers. Moreover, development of a confined-shape bend (caused by artificial barrier or autogenic bend behaviour) may also favour the formation of multiple cutoffs. However, counter migration of meanders enhanced by increased flood frequency and sediment supply are primary triggers for such events. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:许多研究人员已经研究了曲折弯的演变和截断的形成,包括在多个弯道中同时形成的一系列截断。然而,对于导致随后在一个位置上形成的多个截止的发展的因素的了解相对较少。本研究旨在确定曲折弯发展对单个弯道中多个斜槽截止形成的影响。该研究基于低地河流洪泛区(波兰下奥伯河)保留的河曲迁移和截留的沉积记录。进行了曲折几何形状变化的分析,以描述它们的迁移对截留形成的影响以及发生多个截留的其他河流。结果表明,由于上游和下游控制之间的相互作用,近3000年来在奥伯河下游发生了多次截流:河曲弯向相反方向的迁移,伴随着洪水频率和泥沙供应的增加。自19世纪以来,由于人为的影响,水流和泥沙的供应量有了进一步的变化:人为切断下游弯道并抬高了河堤。尽管相比较的河流能量明显较高,但在其他河道中也发现了类似的驱动多重截流形成的机制。此外,受限形状的弯曲(由人工屏障或自发弯曲行为引起)的发展也可能有利于形成多个边界。但是,由于洪水频率增加和沉积物供应增加而使河曲的逆向迁移是此类事件的主要诱因。版权所有(c)2015 John Wiley&Sons,Ltd.

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