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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Rates, distributions and mechanisms of change in meander morphology over decadal timescales, River Dane, UK
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Rates, distributions and mechanisms of change in meander morphology over decadal timescales, River Dane, UK

机译:年代际尺度上蜿蜒形态变化的速率,分布和机制,英国戴恩河

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This paper analyses types and rates of change in river meander morphology and the links between mechanisms of change and emergent behaviour of planform morphology. It uses evidence of four dates of aerial photography combined with annual field mapping and ground photography to examine the morphological changes and mechanisms of change in a series of bends on an active meandering river, the River Dane in NW England, over a 25 year period. This unique data set allows insight into the spatial and temporal variability of bank line movement and component processes. Bank lines were mapped photogrametrically from air photos of 1984, 1996, 2001 and 2007 and the digitised courses compared in ArcGIS to produce calculations of erosional and depositional areas and rates. Most bends exhibit morphological change that largely follows the autogenic sequence, identified in qualitative models of meander development, from low sinuosity curves through simple symmetric and asymmetric bends to compound forms with lobe development in the apex region. Rates of erosion and bankline movement increase through this sequence until the compound phase. Relationships of amounts of movement to various curvature measures of bend morphology are complex. Several new loops, distinct from compound bend behaviour, have developed during the study period in formerly straight sections. Mechanisms of morphological change are illustrated for four types of bends: new, rapid growth bend; sharp-angled bend with mid-channel bar development; symmetric migrating bend; and simple to compound bend development. The changes take place in phases that are not simply related to discharge but to inherent sequences and feedbacks in development of bars and bend morphology and timescales for these are identified. Overall, emergent behaviour of systematic planform change, moderated by channel confinement and boundary features, is produced from spatially and temporally varied channel processes.
机译:本文分析了河曲形态的变化类型和变化速率,以及变化机制与平面形态的涌现行为之间的联系。它使用航空摄影的四个日期的证据与年度野外制图和地面摄影相结合的方法,研究了一条活跃的蜿蜒河(英格兰西北部的戴恩河)在25年内的一系列弯道的形态变化和变化机制。这个独特的数据集可以洞悉堤岸线移动和组成过程的时空变化。从1984年,1996年,2001年和2007年的空中照片通过照相法绘制了河岸线,并在ArcGIS中对数字化路线进行了比较,以得出侵蚀和沉积面积和速率的计算结果。大多数弯头的形态变化在很大程度上遵循自发序列,在蜿蜒发育的定性模型中确定,从低弯曲度曲线到简单的对称和非对称弯头,到在顶点区域具有叶瓣发育的复合形式。腐蚀和堤岸运动的速率在整个过程中一直增加,直到复合阶段为止。移动量与弯曲形态的各种曲率度量之间的关系很复杂。在研究期间,在以前的直线段中出现了几个不同于复合弯曲行为的新环。说明了四种类型的弯曲的形态变化机制:新的快速生长弯曲;弯曲,弯曲和弯曲。尖角弯曲,带有中槽钢筋;对称迁移弯曲并且易于复合弯曲的开发。变化发生的阶段不仅与放电有关,而且还与钢筋的固有序列和反馈有关,并确定了弯曲的形态和时间尺度。总体而言,系统的平面变化的紧急行为是由通道限制和边界特征调节的,它是由时空变化的通道过程产生的。

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