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首页> 外文期刊>Physics Reports: A Review Section of Physics Letters (Section C) >Rayleigh–Taylor and Richtmyer–Meshkov instability induced flow, turbulence, and mixing. II
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Rayleigh–Taylor and Richtmyer–Meshkov instability induced flow, turbulence, and mixing. II

机译:Rayleigh-Taylor和Richtmyer-Meshkov不稳定诱导流动,湍流和混合。 二

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AbstractRayleigh–Taylor (RT) and Richtmyer–Meshkov(RM) instabilities are well-known pathways towards turbulent mixing layers, in many cases characterized by significant mass and species exchange across the mixing layers (Zhou, 2017.Physics Reports, 720–722, 1–136). Mathematically, the pathway to turbulent mixing requires that the initial interface be multimodal, to permit cross-mode coupling leading to turbulence. Practically speaking, it is difficult to experimentally produce a non-multi-mode initial interface. Numerous methods and approaches have been developed to describe the late, multimodal, turbulent stages of RT and RM mixing layers. This paper first presents the initial condition dependence of RT mixing layers, and introduces parameters that are used to evaluate the level of “mixedness” and “mixed mass” within the layers, as well as the dependence on density differences, as well as the characteristic anisotropy of this acceleration-driven flow, emphasizing some of the key differences between the two-dimensional and three-dimensional RT mixing layers. Next, the RM mixing layers are discussed, and differences with the RT mixing layer are elucidated, including the RM mixing layers dependence on the Mach number of the initiating shock. Another key feature of the RM induced flows is its response to a reshock event, as frequently seen in shock-tube experiments as well as inertial confinement events. A number of approaches to modeling the evolution of these mixing layers are then described, in order of increasing complexity. These include simple buoyancy–drag models, Reynolds-averaged Navier–Stokes models of increased complexity, including
机译:<![cdata [ Abstract Rayleigh-Taylor(RT)和RichTmyer-Meshkov(RM)不稳定性是众所周知的湍流混合层的途径,在许多情况下以显着为特征质量和物种在混合层交换(周,2017. 物理报告,720-722,1-136)。在数学上,湍流混合的途径要求初始界面是多模式的,以允许跨模式耦合导致湍流。实际上,难以通过实验产生非多模初始界面。已经开发了许多方法和方法来描述RT和RM混合层的晚期,多模式,湍流阶段。本文首先呈现了RT混合层的初始条件依赖性,并引入了用于评估层内“混合性”和“混合质量”的参数,以及对密度差异的依赖性,以及特征这种加速驱动流的各向异性,强调了二维和三维RT混合层之间的一些关键差异。接下来,讨论RM混合层,阐明与RT混合层的差异,包括RM混合层依赖于起始冲击的马赫数。 RM诱导流的另一个关键特征是其对Reshock事件的响应,如震炮实验中经常看到的以及惯性监禁事件。按照越来越复杂性的顺序描述,将许多用于建模这些混合层的进化的方法。其中包括简单的浮力 - 拖动模型,reynolds-passventaged的Navier-Stokes模型增加了复杂性,包括

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