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Dam-Break Flow on Mobile Bed Through an Idealized City: Numerical Study

机译:移动河床通过理想化城市的溃坝流:数值研究

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Abstract This paper presents a numerical simulation of a three-phase flow (water, air, and mud) formed during a dam break. For the connection between all phases, the mathematical model was modified to take into account the non-Newtonian and Newtonian fluids. The equations in the mathematical model are discretized by the finite volume method and the relationship between all phases is achieved using the volume of fluid (VOF) method. Modified Navier–Stokes equations for accounting for non-Newtonian and Newtonian fluids are solved by the Pressure-Implicit with Splitting of Operators (PISO) numerical algorithm. To validate the mathematical model and numerical algorithm, the paper demonstrates a comparative analysis of the results with the laboratory experiment. The model tested in this way has confirmed its reliability, accuracy and reasonableness. Additionally, a three-dimensional numerical simulation of the water flow movement in combination with a sedimentary layer in a narrowing channel was considered. A rough estimate of the mud flow behavior in relation to the urbanized area located at the end of the channel is given. When analyzing the numerical results, it can be concluded that an increase in the height of the mud layer leads to a deceleration of the moving flow, which can subsequently be used for the timely evacuation of the population. It should be noticed that the analysis of the comparative graphs showed the deceleration of the water flow by more than 0.2?s for a moving layer depth of 0.025?m and when using a mixed arrangement of the sediment. And also from the obtained results, we can note at least two times decrease in the maximum pressure value that in the presence of sediments.
机译:摘要 对溃坝过程中形成的三相流(水、气、泥)进行了数值模拟。对于所有相之间的联系,对数学模型进行了修改,以考虑非牛顿流体和牛顿流体。数学模型中的方程采用有限体积法离散化,各相之间的关系采用流体体积法(VOF)实现。修正的纳维-斯托克斯方程用于计算非牛顿流体和牛顿流体,采用压隐式算子分裂(PISO)数值算法求解。为了验证数学模型和数值算法的有效性,本文对结果进行了与室内实验的对比分析。以这种方式测试的模型证实了其可靠性、准确性和合理性。此外,还考虑了水流运动与沉积层在狭窄河道中的三维数值模拟。给出了与位于河道末端的城市化地区相关的泥石流行为的粗略估计。在分析数值结果时,可以得出结论,泥层高度的增加导致移动流减速,随后可用于及时疏散人口。应该注意的是,对比图的分析显示水流的减速超过0。2?s,对于0.025?m的移动层深度,以及当使用混合排列的沉积物时。而且从获得的结果中,我们可以注意到在存在沉积物的情况下,最大压力值至少降低了两倍。

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