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According to the theory of the stochastic trajectory model of particle in the gas-solid two-phase flows, the two-phase turbulence model between the blades in the inner cavity of the FW-Φ150 horizontal turbo classifier was established, and the commonly-used PHOENICS code was adopted to carried out the numerical simulation. It was achieved the flow characteristics under a certain condition as well as the motion trace of particles with different diameters entering from certain initial location and passing through the flow field between the blades under the correspondent condition. This research method quite directly demonstrates the motion of particles. An experiment was executed to prove the accuracy of the results of numerical simulation.

参考文献

[1] Lu Shouci.Powder Processing Technology[M].北京:中国轻工业出版社,1999:282.
[2] XIE Quanmin,ZHU Ruigen,CHENG Kong.GREY CLASSIFICATION FOR EVALUATING THE STABILITY OF DANGEROUS ROCK-BLOCK MASSES[J].武汉理工大学学报(材料科学版)英,2000(01):73-77.
[3] Zennosuke TANAKA;Masahiko UCHIYAMA .The Accurate Air Classification of Fine Particles[J].粉体工学会誌,1996(4):248-252.
[4] Rachel Anna.Centrifugal Air Classification of the Particles Using Rotating Disks[J].University of Florida,2001
[5] SPALDING D B.The Phoenics Encyclopedia[M].London CHAM Ltd,1994
[6] Zhou Lixing.Dynamics of Multiphase Turbulent Reacting Fluid Flows[M].北京:国防工业出版社,1982
[7] Cen kefa.Fan Jianren.Theory and Calculation for Engineering-oriented Gas-solid Multiphase Flows[M].杭州:浙江大学出版社,1990
[8] 袁宁,张振家.涡轮发动机复杂区域的结构化网格生成技术[J].推进技术,2001(04):311-314.
[9] C Bludszuweit .Three-dimensional Numerical Prediction of Stress Loading of Blood Particles in a Centrifugal Pump[J].Journal of Artificial Organs,1995,19(07):590-596.
[10] D Landwehr;M H Pahl .Comminution Processes in a Tuebo-mill-Part 1[J].Aufbereitungs-Technik,1987,28(02):57-65.
[11] LI Guo-hua,HUANG Zhi-chu,ZHANG You-lin.Specific Property of Ultrafine Particle Classification[J].武汉理工大学学报(材料科学版)英,2003(02):82-84.
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