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Experimental and numerical modeling to investigate the riverbank’s stability

机译:试验和数值模型,调查河岸稳定性

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The purpose of this paper is to assess the failure mechanism of riverbanks due to stream flow experimentally and numericallyto avoid recurring landslides by identifying the most dangerous place and treating them by a suitable method. Theexperiments and the physical models were carried out to study the failure mechanism of riverbank and evaluation oftheir stability in two cases: short-term condition and long-term condition flow where three models were tested. The TigrisRiver (Iraq) is considered as a model in this paper in terms of the applied velocity and modeled soil of the banks it wasused at the same characteristics in the prototype scale. Also, a numerical simulation was performed using the FLOW-3Dprogram to determine the velocity distribution and to identify the areas subjected to the high stress levels through thewater flow. The obtained results in this paper are inspecting of failure mechanism types that occur under the influenceof specific limits of flow velocity, which have shown good compatibility with the type of failure in the prototype scale. Inaddition to calculating the amount of soil erosion, the failure angle, and the amount of soil settlement at the riverbankmodel is investigated also. The results of experimental work and numerical simulation were well matched, where thestandard error rate for Froude number ranged between (1.8%–6.6%), and the flow depth between (2.7%–6.9%).
机译:本文的目的是评估河岸的故障机制由于流动流动实验和数值避免通过识别最危险的地方并通过合适的方法处理它们来重复山体滑坡。这进行实验和物理模型,以研究河岸的失效机制和评价他们在两种情况下的稳定性:短期状况和长期条件流动,其中测试了三种模型。底格里斯河(伊拉克)在本文中被认为是本文的模型,而是它的应用速度和建模土壤在原型规模中使用的相同特征。此外,使用流量3D执行数值模拟确定速度分布的程序,并通过识别通过的高应力水平的区域水流。本文获得的结果是在影响下发生的故障机制类型流速的特定限制,这表明了与原型刻度中的故障类型的良好兼容性。在除了计算土壤侵蚀的量,失败角度和河岸的土壤沉降量模型也被调查了。实验工作的结果和数值模拟非常匹配,其中FRoude号码的标准错误率(1.8%-6.6%),流量深度(2.7%-6.9%)。

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