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Modeling of aerosol formation in a turbulent jet with the transported population balance equation-probability density function approach

机译:运移人口平衡方程-概率密度函数方法对湍流射流中气溶胶形成进行建模

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摘要

Processes involving particle formation in turbulent flows feature complex interactions between turbulence and the various physicochemical processes involved. An example of such a process is aerosol formation in a turbulent jet, a process investigated experimentally by Lesniewski and Friedlander [Proc. R. Soc. London, Ser. A454, 2477 (1998)]. Polydispersed particle formation can be described mathematically by a population balance (also called general dynamic) equation, but its formulation and use within a turbulent flow are riddled with problems, as straightforward averaging results in unknown correlations. In this paper we employ a probability density function formalism in conjunction with the population balance equation (the PBE-PDF method) to simulate and study the experiments of Lesniewski and Friedlander. The approach allows studying the effects of turbulence-particle formation interaction, as well as the prediction of the particle size distribution and the incorporation of kinetics of arbitrary complexity in the population balance equation. It is found that turbulence critically affects the first stages of the process, while it seems to have a secondary effect downstream. While Lesniewski and Friedlander argued that the bulk of the nucleation arises in the initial mixing layer, our results indicate that most of the particles nucleate downstream. The full particle size distributions are obtained via our method and can be compared to the experimental results showing good agreement. The sources of uncertainties in the experiments and the kinetic expressions are analyzed, and the underlying mechanisms that affect the evolution of particle size distribution are discussed.
机译:湍流中涉及颗粒形成的过程具有湍流与所涉及的各种物理化学过程之间复杂的相互作用。这种过程的一个例子是湍流喷射中的气溶胶形成,该过程由Lesniewski和Friedlander [Proc。 R. Soc。伦敦,序列A454,2477(1998)]。多分散颗粒的形成可以用种群平衡(也称为一般动力学)方程进行数学描述,但是在湍流中其形成和使用存在很多问题,因为直接求平均值会导致未知的相关性。在本文中,我们将概率密度函数形式化与人口平衡方程(PBE-PDF方法)结合使用,以模拟和研究Lesniewski和Friedlander的实验。该方法允许研究湍流-颗粒形成相互作用的影响,以及对粒度分布的预测以及在种群平衡方程中纳入任意复杂性的动力学。发现湍流严重影响过程的第一阶段,而下游似乎具有次要作用。尽管Lesniewski和Friedlander认为,大部分成核发生在初始混合层中,但我们的结果表明,大多数颗粒都在下游成核。通过我们的方法可以获得完整的粒径分布,并且可以与显示出良好一致性的实验结果进行比较。分析了实验中的不确定性来源和动力学表达式,并讨论了影响粒度分布演变的潜在机理。

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