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HIGHLIGHTS ON HIGH FLOOD EFFECTS ON RIVER NILE

机译:尼罗河上高洪水影响的亮点

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The flood is a natural phenomenon defined as relatively high flow or stage in a river markedly higher than the usual. It occurs often quite frequently in almost all rivers in the world as a result of a variety of causes. Aswan High Dam (AHD) represents a safeguard for Egypt against high and low floods for more than thirty years. However, Egypt has experienced many high floods during the past few years; examples of them were the floods of 1988, 1998 and 2000. In these floods, the Ministry of Water Resources and Irrigation (MWRI) had to release more discharge downstream the dam to manage the flood and to verify the dam operation restrictions in terms of (water level upstream the dam in the first of Aug. =175.00 m). These releases caused many troubles for human properties and habitations especially in the area of encroachment. In addition, many other side effects on the river behavior, such as aggradations, degradation, bank erosion and many areas were been subjected to inundation. These releases also, indicate some adverse effects on free surface drains. The main purpose of this paper is to introduce the main feature of 1998 flood as an example of high floods. Water surface profiles in critical reaches especially the most downstream reaches are investigated. The reach located between Assiut and Delta Barrages is selected for this investigation. 1 -D Mathematical model (HEC-RAS) is applied to test the effect of increasing the release downstream AHD by applying different scenarios. For each scenario, the water level is predicted, its effect on bank erosion, land inundations, and free drains are analyzed and evaluated. Finally, the study introduces some lessons learned from this flood as well as some recommendations for new flood strategy to manage and limit flood hazards. In addition, some protection and mitigation methods to reduce the potential of floods are also produced.
机译:洪水是一种自然现象,定义为河流中相对较高的流量或舞台,明显高于通常的河流。由于各种原因,它通常在世界上几乎所有的河流中经常发生。阿斯旺高坝(AHD)代表埃及抵御高度和低洪水超过三十年的保障措施。然而,埃及在过去几年中经历了许多高洪水;他们的例子是1988年,1998年和2000年的洪水。在这些洪水中,水资源和灌溉部(MWRI)必须在大坝下游释放更多的放电来管理洪水,并验证大坝运行限制(水位在8月的第一个水位上游达到5月= 175.00米)。这些释放因侵占领域而导致人类性质和居住的许多麻烦。此外,许多关于河流行为的其他副作用,例如泛滥,劣化,银行侵蚀和许多地区都受到淹没。这些版本也表明了对自由表面排水管的一些不利影响。本文的主要目的是介绍1998年洪水的主要特征,是高洪水的一个例子。调查了临界危急达到的水面曲线特别是最下游达到的困境。选择在Assiut和Delta屏障之间的覆盖范围进行该调查。应用了1 -D数学模型(HEC-RAS)以测试通过应用不同场景增加释放下游AHD的效果。对于每种情况,预测水位,分析并评估其对银行侵蚀,土地淹没和自由排水的影响。最后,该研究介绍了从这次洪水中吸取的一些经验教训,以及一些新的洪水战略的建议,以管理和限制洪水危险。此外,还生产了一些保护和缓解方法,以减少洪水潜力。

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