挟沙水流紊动结构  

Turbulent structure of sediment - laden flow

作　　者：万声淦[1] 窦国仁[1] 

机构地区：[1]南京水利科学研究院

出　　处：《水利水运科学研究》1995年第1期89-102,共14页

摘　　要：挟沙水流的紊动结构是十分复杂的研究课题。本文中首先综述了有关清水水流的紊动结构中有代表性的几种研究途径及其存在的问题，进而对挟沙水流的紊动结构进行了综合评述。The turbulent structure of a sediment - laden flow is of high complicated feature and has been attracting attentions of many researchers in the world. The essentials are based on the nonlinear interaction between liquid - phase and solid - phase also among particles.The turbulent structure of clear flow is of fundamental importance, some typical approaches, ie. the statistical theory, the semi - empirical, the coherent structure and the stochastic theory, are systematized in detail. The conventional approaches of the turbulent structure of the sediment - laden flow may be divided as two different ways.The two approaches mentioned above and their important statements and results are also discussed in this article.

关 键 词：泥沙 挟沙水流 紊流 紊流结构 

分 类 号：TV143.4[水利工程—水力学及河流动力学]