Applied Mathematics and Mechanics (English Edition) ›› 2009, Vol. 30 ›› Issue (2): 153-162 .

• Articles • 上一篇    下一篇

Large eddy simulation of turbulent statistical and transport properties in stably stratified flows

  1. 邱翔
  2. 黄永祥
  3. 卢志明
  4. 刘宇陆
  

    1. Shanghai Institute of Applied Mathematics and Mechanics, Shanghai University
    2. Department of Mathematics, School of Sciences,Shanghai University,Shanghai 200444, P. R. China
  • 收稿日期:2008-06-25 修回日期:2008-11-14 出版日期:2009-02-11 发布日期:2009-02-11
  • 通讯作者: 刘宇陆

Large eddy simulation of turbulent statistical and transport properties in stably stratified flows

Xiang QIU,Yong-xiang HUANG,Zhi-ming LU,Yu-lu LIU   

    1. Shanghai Institute of Applied Mathematics and Mechanics, Shanghai University
    2. Department of Mathematics, School of Sciences,Shanghai University,Shanghai 200444, P. R. China
  • Received:2008-06-25 Revised:2008-11-14 Online:2009-02-11 Published:2009-02-11
  • Contact: Yu-lu LIU

摘要: Three dimensional large eddy simulation (LES) is performed in the investigation of stably stratified turbulence with a sharp thermal interface. Main results are focused on the turbulent characteristic scale, statistical properties, transport properties, and temporal and spatial evolution of the scalar field.Results show that the buoyancy scale increases first, and then goes to a certain constant value. The stronger the mean shear, the larger the buoyancy scale. The overturning scale increases with the flow, and the mean shear improves the overturning scale. The flatness factor of temperature departs from the Gaussian distribution in a fairly large region, and its statistical properties are clearly different from those of the velocity fluctuations in strong stratified cases. Turbulent mixing starts from small scale motions,and then extends to large scale motions.

Abstract: Three dimensional large eddy simulation (LES) is performed in the investigation of stably stratified turbulence with a sharp thermal interface. Main results are focused on the turbulent characteristic scale, statistical properties, transport properties, and temporal and spatial evolution of the scalar field.Results show that the buoyancy scale increases first, and then goes to a certain constant value. The stronger the mean shear, the larger the buoyancy scale. The overturning scale increases with the flow, and the mean shear improves the overturning scale. The flatness factor of temperature departs from the Gaussian distribution in a fairly large region, and its statistical properties are clearly different from those of the velocity fluctuations in strong stratified cases. Turbulent mixing starts from small scale motions,and then extends to large scale motions.

Key words: stratified turbulence, turbulent mixing, turbulent transport, turbulence structure

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