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风沙运动的DPM数值模拟
引用本文:亢力强,郭烈锦. 风沙运动的DPM数值模拟[J]. 工程热物理学报, 2006, 27(3): 441-444
作者姓名:亢力强  郭烈锦
作者单位:西安交通大学动力工程多相流国家重点实验室,西安,710049;西安交通大学动力工程多相流国家重点实验室,西安,710049
摘    要:采用离散颗粒模型对风沙气固两相流动进行了数值计算.在该模型中,采用体平均的Navier-Stokes方程来描述气相的运动,对离散颗粒采用拉格朗日方法模拟,求解颗粒运动方程.采用硬球模型描述颗粒问碰撞作用.计算结果表明,沙粒平均水平速度廓线在0.02 m以上高度可以表示为按对数函数或幂函数规律增加,在0.02 m以下则发生偏离;在大于0.02 m的高度,输沙通量随高度按指数规律衰减,而在地面附近由于颗粒蠕移的影响发生偏离,这与已有文献结果一致。本文的模拟有助于风沙运动规律的研究与掌握。

关 键 词:离散颗粒模型(DPM)  硬球模型  风沙运动
文章编号:0253-231X(2006)03-0441-04
修稿时间:2005-12-04

SIMULATION OF WINDBLOWN SAND MOVEMENT BY DISCRETE PARTICLE MODEL
KANG Li-Qiang,GUO Lie-Jin. SIMULATION OF WINDBLOWN SAND MOVEMENT BY DISCRETE PARTICLE MODEL[J]. Journal of Engineering Thermophysics, 2006, 27(3): 441-444
Authors:KANG Li-Qiang  GUO Lie-Jin
Abstract:Numerical simulation of windblown sand gas-solid two-phase flow is performed with discrete particle model. In the model, the gas phase is described by the volume-aver aged Navier-Stokes equations of two-phase flow. The particle motion is obtained by solving Newton's second law of motion. The hard sphere model is used to describe inter-particle collisions. The results show that, the variation of mean horizontal velocity of the sands with height can be expressed by a logarithmical function or a power function above 0.02 m and shows a deviation below 0.02 m. The sand mass flux decreases exponentially with height above 0.02 m, but there is a deviation from the exponential decay due to the creep grains in the near-bed region. The present simulation is helpful to reveal the mechanism in windblown sand movement.
Keywords:Discrete particle model  hard sphere model  windblown sand movement
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