Numerical Study of Air-Vapor-Particle Flow in Gas Cyclone

被引:0
作者
Jin, Ruizhi [1 ]
Zhao, Ming [1 ]
Zhang, Yumeng [2 ]
Wang, Bo [2 ]
Dong, Kejun [1 ]
机构
[1] Western Sydney Univ, Sch Engn Design & Built Environm, Penrith, NSW 2751, Australia
[2] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China
基金
澳大利亚研究理事会;
关键词
air purification; condensational growth; gas cyclone; particle droplets; vapor condensation; NON-CONDENSABLE GAS; HETEROGENEOUS CONDENSATION; FINE PARTICLES; COLLECTION EFFICIENCY; SUBMICRON PARTICLES; STEAM CONDENSATION; CFD SIMULATION; GROWTH; SEPARATION; PERFORMANCE;
D O I
10.1002/ppsc.202400115
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
This paper presents a numerical study of the complex multiphase flow of air, vapor, and particles in an innovative gas cyclone called CAP cyclone. The air-vapor flow is modeled as a mixture by the Reynolds-averaged Navier-Stokes equations with the mixture species transport and the Eulerian wall film model using FLUENT. Particle flow is modeled by the Lagrangian particle tracking method and the condensational growth of particle droplets is modeled via a user-defined function. The model is validated by reaching good agreement with experimental results. Flow field analysis shows that the added vapor does not change the major vortex characteristics in the cyclone, but the vapor distribution is not uniform. The vapor concentration is much higher in the upper part than in the lower part of the cyclone, leading to insufficient condensational growth in the lower part. A secondary vapor injection is proposed to improve the vapor concentration in the lower part, which is shown to be effective in improving the collection efficiency. The model and the results are helpful to the understanding and optimization of the CAP cyclone technology, and also the vapor and particle droplet flow in turbulent flows. Air-vapor-particle flow in a novel cyclone utilizing condensational growth is numerically studied. The flow field is similar to dry cyclone but vapor is not uniformly distributed. The condensational growth is insufficient in the lower part of the cyclone, which can be remedied by a secondary vapor injection. Vapor flow and condensation in channel flow and vortex flow are also compared. image
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页数:14
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