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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Revisiting the morphological method in two-dimensions to quantify bed-material transport in braided rivers
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Revisiting the morphological method in two-dimensions to quantify bed-material transport in braided rivers

机译:重新审视两维的形态方法,以定量编织河流的床头物质运输

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Research in the 1990s showed that bed-material transport rates could be estimated at the reach scale in both one-dimension and, over small spatial scales (10s of m), in two-dimensions. The limit on the latter was the spatial scale over which it was possible to obtain distributed data on morphological change. Here, we revisit the morphological method given progress in both topographical data acquisition and hydraulic modelling. The bed-material transport needed to conserve mass is calculated in both one and two dimensions for a 1600 m x 300 m Alpine braided river "laboratory". High-resolution topographical data were acquired by laser scanning to quantify Digital Elevation Models (DEMs), and morphological changes caused by the flushing of the water intake were derived from repeated surveys. Based on DEMs of differences, 1D bed-material transport rates were calculated using the morphological method. Then, a 2D hydraulic model was combined with a topographic correction to route sediment through the network of braided channels and to obtain a spatially variable estimate of transport in both downstream and cross-stream directions. Monte Carlo simulation was applied to the routing model parameters, allowing identification of the most probable parameter values needed to minimize negative transport. The results show that within-section spatial compensation of erosion and deposition using the 1D treatment leads to substantial local errors in transport rate estimates, to a degree related to braiding intensity. Even though the 2D application showed that a large proportion of the total transport was actually concentrated into one main channel during the studied low flow event, the proportion of transport in secondary anabranches is substantial when the river starts braiding. Investigations of the effects of DEM resolution, competent flow duration and survey frequency related to 'travelling bedload' and sequential erosion-deposition emphasized the critical importance of careful d
机译:20世纪90年代的研究表明,床头材料运输速率可以在一维的达达尺寸下估计,并且在两维中的小空间尺度(10米)上。后者的限制是可以获得关于形态变化的分布式数据的空间尺度。在这里,我们重新审视了各种地形数据采集和液压建模的进展的形态学方法。需要保护质量的床形式,以1600m x 300 m高山编织河“实验室”计算。通过激光扫描来获得高分辨率的地形数据来量化数字高度模型(DEM),并且通过反复调查来衍生出水摄入量引起的形态变化。基于差异的DEM,使用形态法计算1D床材料传输速率。然后,将2D液压模型与地形校正组合以通过编织通道网络路由沉积物,并在下游和交叉流方向上获得空间可变的运输估计。 Monte Carlo模拟应用于路由模型参数,允许识别最小化负运输所需的最可能的参数值。结果表明,在局部内的空间补偿使用1D处理的腐蚀和沉积导致运输速率估算中的大量局部误差,与编织强度有关的程度。尽管2D应用表明,在学习的低流量事件期间实际集中到一个主频道的大部分总体运输中,但在河流开始编织时,次级人物的运输比例很大。调查DEM解决方案的影响,与“旅行床单”和顺序侵蚀沉积相关的竞争持续时间和调查频率强调了谨慎D的关键重要性

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