论文标题

两流体大涡模拟的有限尺寸校正模型的颗粒边界层流量

A finite-size correction model for two-fluid Large-Eddy Simulation of particle-laden boundary layer flow

论文作者

Mathieu, Antoine, Chauchat, Julien, Bonamy, Cyrille, Balarac, Guillaume, Hsu, Tian-Jian

论文摘要

在本文中,研究了边界层流中的单分散有限大小的固体颗粒的悬浮液,以预测单分散的有限尺寸固体颗粒的悬浮液的能力。对于较重的液流体颗粒,其在床摩擦速度的速度的速度下,两流体模型显着低估了颗粒的湍流分散体。假设有限尺寸的效果很重要,并提出了阻力定律的校正模型。该模型基于以下假设:湍流尺度大于颗粒直径将有助于两个阶段之间分辨的相对速度,而小于颗粒直径的涡流将产生两个效果:(i)它们将减少粒子响应时间,通过增加对阻力系数的质量质量粘度来减少剂量的质量,并增加了(II)的贡献。整合有限尺寸的效果使我们能够定量预测较重的液体颗粒的浓度曲线,而无需任何调整参数。提议的两流体模型的修改扩展了其适用性范围,以应对具有属于惯性湍流范围的粒子,并使我们能够在流动强迫条件下设想更复杂的应用,即薄板流动,波浪流,波动驱动的传输,浊度和/或流动层状和流动地点,即dunes,dunes,dunes,scour,scour。

In this paper the capabilities of the turbulence-resolving Eulerian-Eulerian two-phase flow model to predict the suspension of mono-dispersed finite-sized solid particles in a boundary layer flow are investigated. For heavier-than-fluid particles, having settling velocity of the order of the bed friction velocity, the two-fluid model significantly under-estimates the turbulent dispersion of particles. It is hypothesized that finite-size effects are important and a correction model for the drag law is proposed. This model is based on the assumption that the turbulent flow scales larger than the particle diameter will contribute to the resolved relative velocity between the two phases, whereas eddies smaller than the particle diameter will have two effects: (i) they will reduce the particle response time by adding a sub-particle scale eddy viscosity to the drag coefficient, and (ii) they will contribute to increase the production of granular temperature. Integrating finite-size effects allows us to quantitatively predict the concentration profile for heavier-than-fluid particles without any tuning parameter. The proposed modification of the two-fluid model extends its range of applicability to tackle particles having a size belonging to the inertial range of turbulence and allows us to envision more complex applications in terms of flow forcing conditions, i.e. sheet flow, wave-driven transport, turbidity currents and/or flow geometries, i.e. ripples, dunes, scour.

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