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首页> 外文期刊>Hydrology and Earth System Sciences Discussions >A multi basin SWAT model analysis of runoff and sedimentation in the Blue Nile, Ethiopia
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A multi basin SWAT model analysis of runoff and sedimentation in the Blue Nile, Ethiopia

机译:埃塞俄比亚青尼罗河地区径流与泥沙的多流域SWAT模型分析

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A multi basin analysis of runoff and erosion in the Blue Nile Basin, Ethiopia was conducted to elucidate sources of runoff and sediment. Erosion is arguably the most critical problem in the Blue Nile Basin, as it limits agricultural productivity in Ethiopia, degrades benthos in the Nile, and results in sedimentation of dams in downstream countries. A modified version of the Soil and Water Assessment Tool (SWAT) model was developed to predict runoff and sediment losses from the Ethiopian Blue Nile Basin. The model simulates saturation excess runoff from the landscape using a simple daily water balance coupled to a topographic wetness index in ways that are consistent with observed runoff processes in the basin. The spatial distribution of landscape erosion is thus simulated more correctly. The model was parameterized in a nested design for flow at eight and sediment at three locations in the basin. Subbasins ranged in size from 1.3 to 174 000 kmsup2/sup, and interestingly, the partitioning of runoff and infiltrating flow could be predicted by topographic information. Model predictions showed reasonable accuracy (Nash Sutcliffe Efficiencies ranged from 0.53a??0.92) with measured data across all sites except Kessie, where the water budget could not be closed; however, the timing of flow was well captured. Runoff losses increased with rainfall during the monsoonal season and were greatest from areas with shallow soils and large contributing areas. Analysis of model results indicate that upland landscape erosion dominated sediment delivery to the main stem of the Blue Nile in the early part of the growing season when tillage occurs and before the soil was wetted up and plant cover was established. Once plant cover was established in mid August landscape erosion was negligible and sediment export was dominated by channel processes and re-suspension of landscape sediment deposited early in the growing season. These results imply that targeting small areas of the landscape where runoff is produced can be the most effective at controlling erosion and protecting water resources. However, it is not clear what can be done to manage channel erosion, particularly in first order streams in the basin.
机译:对埃塞俄比亚青尼罗河盆地的径流和侵蚀进行了多盆地分析,以阐明径流和沉积物的来源。侵蚀可以说是青尼罗河盆地中最关键的问题,因为它限制了埃塞俄比亚的农业生产力,使尼罗河中的底栖生物退化,并导致下游国家大坝的沉积。开发了土壤和水评估工具(SWAT)模型的修改版本,以预测埃塞俄比亚青尼罗河盆地的径流和沉积物损失。该模型使用简单的每日水平衡与地形湿度指数相结合的方式,模拟了景观中的饱和饱和径流,其方式与盆地中观测到的径流过程一致。因此,可以更正确地模拟景观侵蚀的空间分布。该模型采用嵌套设计进行参数化,以实现盆地中8个位置的水流和3个位置的沉积物。子流域的大小从1.3到174 000 km 2 不等,有趣的是,可以通过地形信息预测径流和渗流的分配。模型预测表明,除凯西(Kessie)无法关闭水预算外,所有地点的测量数据都具有合理的准确性(纳什苏特克利夫效率范围为0.53a≤0.92)。然而,流动的时机被很好地捕捉了。在季风季节,径流损失随降雨增加而增加,在土壤浅且贡献大的地区尤为严重。对模型结果的分析表明,在生长季节的初期,当耕作发生时以及在土壤被润湿并建立植物覆盖之前,高地景观侵蚀主导着向尼罗河主要干地的泥沙输送。一旦在8月中旬建立了植物覆盖物,景观侵蚀就可以忽略不计了,沉积物的出口主要由河道过程和生长季节初期沉积的景观沉积物的再悬浮所决定。这些结果表明,针对产生径流的小区域景观,在控制侵蚀和保护水资源方面最有效。但是,目前尚不清楚可以采取什么措施来治理河道侵蚀,特别是在盆地一级流中。

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