期刊文献+

基于DANS方程的粗糙床面明渠水力特性研究 被引量:3

Research on hydraulic characteristics of open-channel flow over rough bed based on DANS equations
下载PDF
导出
摘要 基于双向平均NS方程(DANS方程)建立粗糙床面明渠水流数学模型,应用修正的S-A湍流模型对其紊流过程进行模拟,采用涡黏系数法计算明渠湍流在粗糙床面上存在障碍物时的形状应力,结果表明:形状应力在障碍物层以内不可忽略,而在障碍物上部,会迅速减小直至可忽略不计;速度值会随形状应力的增大而减小;障碍物顶部附近的雷诺应力也会因为形状应力的存在而有明显的减小。此外,针对障碍物孔隙率的研究表明:障碍物孔隙率的分布对速度、雷诺应力及形状应力等存在一定的影响,并且当孔隙率的分布越光滑时,其影响越小。 A numerical model of open-channel flow over a rough bed was established based on double-averaged NS ( DANS) equations. The turbulence was simulated by a modified Spalart-Allmaras ( S-A) turbulence model, and the form-induced stress was calculated with a sub-layer-scale eddy viscosity model. The results show that the form-induced stress within the roughness layer cannot be ignored, and it decreased rapidly with the distance above the top of the roughness layer. The form-induced stress accounted for the dispersion of the velocity profiles and caused a slight reduction of the mean velocity. It also significantly decreased the Reynolds stress at the top of the roughness layer. In addition, this study shows that the velocity profile, the Reynolds stress profile, and the form-induced stress profile are affected by the distribution of the porosity. A smoother profile of porosity has less impact on the flow and turbulence characteristics.
出处 《河海大学学报(自然科学版)》 CAS CSCD 北大核心 2014年第3期217-222,共6页 Journal of Hohai University(Natural Sciences)
基金 国家重点基础研究发展计划(973计划)(2010CB429001)
关键词 DANS方程 形状应力 孔隙率 S-A湍流模型 涡黏系数法 粗糙床面 DANS equations form-induced stress porosity S-A turbulence model eddy viscosity model rough bed
  • 相关文献

参考文献15

  • 1NIKORA V,MCEWAN 1,MCLEAN S,et al.Double-averaging concept for rough-bed open-channel and overland flows:theoretical background[ J].ASCE,Journal of Hydraulic Engineering,2007,133(8):873-883.
  • 2NIKORA V,MCLEAN S,COLEMAN S,et al.Double-averaging concept for rough-bed open-channel and overland flows:applications [ J ].ASCE,Journal of Hydraulic Engineering,2007,133(8):884-895.
  • 3NIKORA V,GORING D,MCEWAN I,et al.Spatially averaged open-channel flow over rough bed [ J ].ASCE,Journal of Hydraulic Engineering,2001,127(2):123-133.
  • 4SMITH J D,MCLEA S R.Spatially averaged flow over a wavy surface [ J ].Journal of Geophysical Research,1977,82(12):1735-1746.
  • 5WILSON N R,SHAW R H.A higher order closure model for canopy flow[ J].Journal of Applied Meteorology and Climatology,1977,16:1197-1205.
  • 6POGGI D,KATUL G G,ALBERTSON J D.A note on the contribution of dispersive fluxes to momentum transfer within canopies [ J ].Boundal3-Layer Meteorology,2000,111:615 4521.
  • 7POGGI D,PORPORATO A,RIDOLFI L,et al.The effect of vegetation density on canopy sub-layer turbulence [ J ].Boundary-Layer Meteorology,2000,111:565-587.
  • 8MCLEAN S,NIKORA V.Characteristics of turbulent unidirectional flow over rough beds:double-averaging perspective with particular focus on sand dunes and gravel beds [J].Water Resources Research,2006,42,W10409,DOI:10.1029/2005WR000708.
  • 9CAMPBELL L,MCEWAN I,NIKORA V,et al.Bed load effects on hydrodynamics of rough bed open channel flows [ J ].ASCE,Journal of Hydraulic Engineering,2005,131(7):576-585.
  • 10ABERLE J.Spatially averaged near-bed flow field over rough armor layers[ C]//ELSA C T,CARDOSO A H,LEAL J G,et al.Proceedings of the International Conference on Fluvial Hydraulics.Lisbon,Portugal:Taylor & Francis,2006:153-162.

同被引文献24

引证文献3

二级引证文献7

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部