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Numerical Investigation of Sand-Bed Erosion by an Upward Water Jet

机译:向上水射流的砂床侵蚀的数值调查

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A numerical model based on computational fluid dynamics and kinetic theory of granular material is used to investigate sand-bed erosion due to an upward water jet. After verifying the numerical model, the onset and mechanism of the sand-bed erosion are analyzed. As the the inlet water-jet velocity increases, a cavity around the jet orifice is first formed by the water jet, and the sand bed is eroded with a significant expansion. The numerical simulation shows that the increase in sand particle size and sand-bed height can significantly increase the inlet water velocity, causing sand-bed erosion. In addition, the critical velocity leading to sand-bed erosion is decreased as the sand friction angle decreases. Based on the observation and analysis of the numerical simulation, an analytical model using force equilibrium analysis and Ergun's equation is proposed. The interaction between the mobilized and static zones in the sand bed is taken into account using granular theory. The critical inlet water velocity leading to the sand-bed erosion can be determined using this analytical model. This study provides a fundamental understanding of the mechanism of sand-bed erosion, and this numerical technique is shown to be an effective and promising way to investigate sand-bed behavior under an upward water jet. (C) 2017 American Society of Civil Engineers.
机译:采用基于计算流体力学和颗粒材料动力学理论的数值模型,研究了向上射流对砂层的侵蚀。在对数值模型进行验证后,分析了砂层侵蚀的发生和机理。随着进水射流速度的增加,射流首先在喷孔周围形成空腔,砂层被侵蚀并显著膨胀。数值模拟表明,砂粒尺寸和砂床高度的增加会显著提高进水流速,导致砂床侵蚀。此外,导致砂层侵蚀的临界速度随着砂土摩擦角的减小而减小。基于对数值模拟的观察和分析,提出了一种基于力平衡分析和Ergun方程的分析模型。利用颗粒理论,考虑了砂层中活动区和静态区之间的相互作用。利用该分析模型可以确定导致砂层侵蚀的临界进水速度。这项研究为砂层侵蚀机理提供了一个基本的理解,并且该数值技术被证明是研究向上喷水条件下砂层行为的一种有效且有希望的方法。(C) 2017年美国土木工程师学会。

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